Sarmila/GeoWiki-Features huggingface dataset:
This is one of the best exposed and largest calderas in the world; the largest caldera known is Toba in Sumatra with a maximum length of. La Pacana might not be a single caldera; some reconstructions imply that the northern parts of the caldera are actually a separate collapse structure. The floor of the caldera lies at an elevation of, the central uplift and the caldera rim are higher and reach.

Geographic entities mentioned:
surface_form: la pacana
instance_of: Mountain
countries: Chile
coordinates: lat: -23.16666667
lon: -67.41666667
surface_form: pacana
instance_of: Mountain
countries: Chile
coordinates: lat: -23.16666667
lon: -67.41666667
The caldera rim is well exposed except in the northern and western sides, where later volcanism has buried it. After the formation of the caldera, sediments and tuffs within the caldera were uplifted over an angular area of, forming the high resurgent dome known as Cordón La Pacana. This resurgent dome is cut by numerous faults and features a poorly developed graben on its summit.

Geographic entities mentioned:
surface_form: la pacana
instance_of: Mountain
countries: Chile
coordinates: lat: -23.16666667
lon: -67.41666667
surface_form: pacana
instance_of: Mountain
countries: Chile
coordinates: lat: -23.16666667
lon: -67.41666667
Stratovolcanoes inside the caldera include the cones associated with the Cerros de Guayaques lava domes and the volcanoes Cerro Incaguasi, Cerros de Pili, Cerros Negros and Huailitas. Some extant hot springs within the caldera may indicate that there is still a geothermal system associated with La Pacana, although not a very important one considering their low temperature (less than).

Geographic entities mentioned:
surface_form: la pacana
instance_of: Mountain
countries: Chile
coordinates: lat: -23.16666667
lon: -67.41666667
surface_form: pacana
instance_of: Mountain
countries: Chile
coordinates: lat: -23.16666667
lon: -67.41666667
Streams such as Río de Pili and Río Salado complete the hydrology of the caldera. Gravimetric observations have been conducted on La Pacana. A large negative anomaly (an anomaly with less-than-expected mass crust) coincides with the surface of the La Pacana caldera and extends past its borders; it may be a consequence of the caldera being infilled with low-density material.

Geographic entities mentioned:
surface_form: la pacana
instance_of: Mountain
countries: Chile
coordinates: lat: -23.16666667
lon: -67.41666667
surface_form: pacana
instance_of: Mountain
countries: Chile
coordinates: lat: -23.16666667
lon: -67.41666667
Streams such as Río de Pili and Río Salado complete the hydrology of the caldera. Gravimetric observations have been conducted on La Pacana. A large negative anomaly (an anomaly with less-than-expected mass crust) coincides with the surface of the La Pacana caldera and extends past its borders; it may be a consequence of the caldera being infilled with low-density material.

Geographic entities mentioned:
surface_form: la pacana
instance_of: Mountain
countries: Chile
coordinates: lat: -23.16666667
lon: -67.41666667
surface_form: pacana caldera
instance_of: Mountain
countries: Chile
coordinates: lat: -23.16666667
lon: -67.41666667
Later the San Bartolo and Silapeti groups were generated, ending by the early Pleistocene. Volcanic activity at La Pacana is more recent than elsewhere in the region, with the oldest volcanic rocks that crop out in La Pacana being between 11 and 7.5 million years old. Large scale ignimbritic activity continued until 2 million years ago. Regional.

Geographic entities mentioned:
surface_form: la pacana
instance_of: Mountain
countries: Chile
coordinates: lat: -23.16666667
lon: -67.41666667
surface_form: la pacana
instance_of: Mountain
countries: Chile
coordinates: lat: -23.16666667
lon: -67.41666667
surface_form: pacana
instance_of: Mountain
countries: Chile
coordinates: lat: -23.16666667
lon: -67.41666667
surface_form: pacana
instance_of: Mountain
countries: Chile
coordinates: lat: -23.16666667
lon: -67.41666667
Local. The basement beneath La Pacana is formed by sediments of Ordovician age, Devonian-Permian quartzites, the mixed Salta formation also of Permian age and sediments of Cretaceous-Tertiary age. At the eastern margin of La Pacana in Argentina, they overlay an even older Precambrian basement.

Geographic entities mentioned:
surface_form: la pacana
instance_of: Mountain
countries: Chile
coordinates: lat: -23.16666667
lon: -67.41666667
surface_form: pacana
instance_of: Mountain
countries: Chile
coordinates: lat: -23.16666667
lon: -67.41666667
At the eastern margin of La Pacana in Argentina, they overlay an even older Precambrian basement. Most of this original basement however is covered by Miocene ignimbrites from centres that may coincide with the La Pacana caldera. Two of these older ignimbrites are known as the Pampa Múcar and Antigua Chacaliri ignimbrites.

Geographic entities mentioned:
surface_form: la pacana
instance_of: Mountain
countries: Chile
coordinates: lat: -23.16666667
lon: -67.41666667
surface_form: pacana caldera
instance_of: Mountain
countries: Chile
coordinates: lat: -23.16666667
lon: -67.41666667
Guacha experienced two major eruptions, of which one occurred 4.1 million years ago. The Purico complex began erupting 1.3 million years ago; it is the youngest centre of the La Pacana Complex with the youngest eruptions occurring during the Holocene. Additional volcanic centres west and southwest of La Pacana are Acamarachi, Láscar, Colachi and Cordón de Puntas Negras.

Geographic entities mentioned:
surface_form: la pacana
instance_of: Mountain
countries: Chile
coordinates: lat: -23.16666667
lon: -67.41666667
surface_form: pacana
instance_of: Mountain
countries: Chile
coordinates: lat: -23.16666667
lon: -67.41666667
Additional volcanic centres west and southwest of La Pacana are Acamarachi, Láscar, Colachi and Cordón de Puntas Negras. A number of faults transect the region at La Pacana, including the north-south Miscanti Lineament and the Socompa and Quisiquiro lineaments.

Geographic entities mentioned:
surface_form: la pacana
instance_of: Mountain
countries: Chile
coordinates: lat: -23.16666667
lon: -67.41666667
surface_form: pacana
instance_of: Mountain
countries: Chile
coordinates: lat: -23.16666667
lon: -67.41666667
Not all of these minerals are found in both ignimbrites, and not always in the same phase (crystals or matrix). Ultimately, the magmas at La Pacana are the products of mantle melts interacting with various crustal domains deep in the crust, within the partially molten zone that has been found at depths of beneath the Altiplano-Puna volcanic complex.

Geographic entities mentioned:
surface_form: la pacana
instance_of: Mountain
countries: Chile
coordinates: lat: -23.16666667
lon: -67.41666667
surface_form: pacana
instance_of: Mountain
countries: Chile
coordinates: lat: -23.16666667
lon: -67.41666667
Also, some of the ignimbrites erupted by La Pacana originally were attributed to Cerro Guacha. Both ignimbrites originated from different parts of the same magma chamber and their origin in the La Pacana caldera is established by isotope ratios of the rocks and the geographical distribution of their outcrops.

Geographic entities mentioned:
surface_form: la pacana
instance_of: Mountain
countries: Chile
coordinates: lat: -23.16666667
lon: -67.41666667
surface_form: pacana caldera
instance_of: Mountain
countries: Chile
coordinates: lat: -23.16666667
lon: -67.41666667
Both ignimbrites originated from different parts of the same magma chamber and their origin in the La Pacana caldera is established by isotope ratios of the rocks and the geographical distribution of their outcrops. Pyroclastic deposits in the Eastern Cordillera of Argentina may have their origin at La Pacana.

Geographic entities mentioned:
surface_form: la pacana
instance_of: Mountain
countries: Chile
coordinates: lat: -23.16666667
lon: -67.41666667
surface_form: pacana
instance_of: Mountain
countries: Chile
coordinates: lat: -23.16666667
lon: -67.41666667
The first large eruption, which took place between 4 ± 0.9 and 5.3 ± 1.1 million years ago, formed the Toconao ignimbrite. The Toconao ignimbrite crops out mainly west of the caldera; only later were units of the Toconao identified on the eastern side of La Pacana. This ignimbrite has a volume of approximately and is formed by a lower un-indurated and an upper indurated subunit.

Geographic entities mentioned:
surface_form: la pacana
instance_of: Mountain
countries: Chile
coordinates: lat: -23.16666667
lon: -67.41666667
surface_form: pacana
instance_of: Mountain
countries: Chile
coordinates: lat: -23.16666667
lon: -67.41666667
Tube pumices are contained in the lower subunit and in a less than Plinian deposit that was emplaced beneath the Toconao ignimbrite. The formation of the caldera coincided with the eruption of the Atana ignimbrite; the eruption was still underway when the terrain subsided to a depth of beneath the previous surface in the northwestern segment of La Pacana.

Geographic entities mentioned:
surface_form: la pacana
instance_of: Mountain
countries: Chile
coordinates: lat: -23.16666667
lon: -67.41666667
surface_form: pacana
instance_of: Mountain
countries: Chile
coordinates: lat: -23.16666667
lon: -67.41666667
This ignimbrite is considerably larger than the Toconao ignimbrite, reaching a volume of and a volcanic explosivity index of 8. This makes the Atana eruption the fifth-largest explosive eruption known and La Pacana a supervolcano. The Atana ignimbrite forms a flow sheet that extends from within the caldera to the outside in the form of a thick structure.

Geographic entities mentioned:
surface_form: la pacana
instance_of: Mountain
countries: Chile
coordinates: lat: -23.16666667
lon: -67.41666667
surface_form: pacana
instance_of: Mountain
countries: Chile
coordinates: lat: -23.16666667
lon: -67.41666667
This separate ignimbrite was christened to be an upper and a lower Tara ignimbrite, possibly erupted by the Cerro Guacha caldera. The Tara ignimbrite fills part of the La Pacana caldera. The total volume of the La Pacana ignimbrites proper is estimated to be about, on the basis of gravimetric information about the volume of the caldera and the infill ignimbrites.

Geographic entities mentioned:
surface_form: la pacana
instance_of: Mountain
countries: Chile
coordinates: lat: -23.16666667
lon: -67.41666667
surface_form: pacana caldera
instance_of: Mountain
countries: Chile
coordinates: lat: -23.16666667
lon: -67.41666667
This separate ignimbrite was christened to be an upper and a lower Tara ignimbrite, possibly erupted by the Cerro Guacha caldera. The Tara ignimbrite fills part of the La Pacana caldera. The total volume of the La Pacana ignimbrites proper is estimated to be about, on the basis of gravimetric information about the volume of the caldera and the infill ignimbrites.

Geographic entities mentioned:
surface_form: la pacana
instance_of: Mountain
countries: Chile
coordinates: lat: -23.16666667
lon: -67.41666667
surface_form: pacana
instance_of: Mountain
countries: Chile
coordinates: lat: -23.16666667
lon: -67.41666667
It is located in the Sierra de Catorce range, one of the highest plateaus in Mexico, where summits may extend over. These mountains lie in the arid Mexican Plateau, cut off from trade winds of the Gulf of Mexico by the high peaks of the Sierra Madre Oriental. The main road to Real de Catorce leaves Highway 62 between Matehuala and San Tiburcio.

Geographic entities mentioned:
surface_form: Mexican Plateau
instance_of: Plateau
countries: Mexico
coordinates: lat: 24
lon: -103
In 1854, during a conflict with a rival Kyrgyz tribe, Ormon was captured in battle and executed. Ormon's khanate collapsed following his death, with the region falling under Russian control by 1868. Background. Ormon Niyazbek uulu was born around 1792 in the Issyk-Kul valley of Kyrgyzstan. Ormon was a member of the powerful tribe, and his family was very influential in the region.

Geographic entities mentioned:
surface_form: Issyk-Kul
instance_of: Lake
countries: Kyrgyzstan
coordinates: lat: 42.416666666667
lon: 77.25
His great-great-grandfather, Mamatkul Biy, had been a high-ranking &quot;manap&quot; amongst the northern Kyrgyz and was proclaimed khan in 1758. Ormon's grandfather, permanently settled in the Chüy and Talas valleys. However, Ormon's father, Niyazbek, is said to have made &quot;little impression on Sarybagysh memory&quot; besides being the father of Ormon.

Geographic entities mentioned:
surface_form: Chüy
instance_of: Valley
countries: Kyrgyzstan
Kazakhstan
Russian Empire
Soviet Union
coordinates: lat: 42.8333
lon: 75.2833
In 1842, Bukhara invaded Kokand, temporarily occupying the state and executing the khan of Kokand, Muhammad Ali Khan. That summer, the chiefs of the northern Kyrgyz tribes organized a kurultai on the western shore of Issyk-Kul near Kochkor in order to plan how to protect the Kyrgyz tribes from external threats.

Geographic entities mentioned:
surface_form: Issyk-Kul
instance_of: Lake
countries: Kyrgyzstan
coordinates: lat: 42.416666666667
lon: 77.25
During campaigns, the army was accompanied by a military band consisting of a kerney and two surnays. Ormon himself was skilled at playing the komuz. Ormon established his capital in the village of Baisoorun in the Semyonov Gorge. In the 1840s, he had an adobe fortress (&quot;korgon&quot;) constructed at the pass, designing it to be able to protect against internal conflicts.

Geographic entities mentioned:
surface_form: Semyonov Gorge
instance_of: Mountain
countries: Kyrgyzstan
coordinates: lat: 42.274361111111
lon: 80.116
In 1846, Kenesary Khan, the leader of the Kazakh Khanate who was leading a rebellion against the Russian Empire, was forced out of his territory by Russian forces advancing from Orenburg. Kenesary's army retreated to the Zhetysu region, which was on the border with the Kyrgyz tribes in the Chüy and Ili valleys.

Geographic entities mentioned:
surface_form: Chüy
instance_of: Valley
countries: Kyrgyzstan
Kazakhstan
Russian Empire
Soviet Union
coordinates: lat: 42.8333
lon: 75.2833
The exact location of Ormon's body is unknown, as his relatives buried him in secret so his body would not be abused. Ormon is believed to be buried either in a pasture near Semyonovka or above the village of Grigor'yevka in the foothills of the Küngöy Ala-Too Range. In the 2010s, Ormon's descendants installed a small monument in the pasture.

Geographic entities mentioned:
surface_form: Küngöy Ala-Too Range
instance_of: Mountain
countries: Kyrgyzstan
coordinates: lat: 42.776166
lon: 76.690021
Dupleix next entered into negotiations about the subjugation of southern India. He sent a large body of troops to the aid of the two claimants of the sovereignty of the Carnatic and the Deccan. The British sided with their rivals to prevent the plans of Dupleix from materializing. In 1750 the Subadar of Deccan gifted the Alamparai Fort to the French.

Geographic entities mentioned:
surface_form: Deccan
instance_of: Plateau
countries: India
coordinates: lat: 15
lon: 77
With Thomas pulling clear of Jungels, Nairo Quintana () countered to the group of pursuers; Thomas was able to stay clear until the end, winning the stage by nine seconds from Tom Dumoulin of. Thomas finished second on stage 4 to Monte Terminillo, 18 seconds behind Nairo Quintana of (). He finished fifth overall, 58 seconds behind Quintana.

Geographic entities mentioned:
surface_form: Monte Terminillo
instance_of: Mountain
countries: Italy
coordinates: lat: 42.47327
lon: 12.99732
At the Tour de France, Thomas won the opening stage, a individual time trial, making him the first Welsh rider to wear the yellow jersey in the event. He held the yellow jersey until Stage 5, when he dropped to second overall behind teammate Chris Froome after finishing tenth on La Planche des Belles Filles.

Geographic entities mentioned:
surface_form: La Planche des Belles Filles
instance_of: Mountain
countries: France
coordinates: lat: 47.7672
lon: 6.77417
Thomas assumed the race lead following a positive COVID-19 test for Evenepoel, a lead he held for four stages, before Bruno Armirail assumed the pink jersey after the peloton lost more than twenty minutes on stage fourteen. Thomas retook the race lead two stages later after Armirail cracked on the final climb to Monte Bondone.

Geographic entities mentioned:
surface_form: Monte Bondone
instance_of: Mountain
countries: Italy
coordinates: lat: 45.98805556
lon: 11.03083333
They ruled the village in an acceptable manner but over the time the family line ended, there was only a mother and son left. One day, the mother and son went to the Kaveri river to pray for their deceased relatives. On their way back to the village, they saw from the Gadikuzhi hills some soldiers of the ruler of Chirakkal town taking Kunhimangalam. The mother and son ended their life in fire.

Geographic entities mentioned:
surface_form: Kaveri
instance_of: Watercourse
countries: India
coordinates: lat: 11.370345
lon: 79.828105
Ithaca campus. Cornell University's main campus is located in Ithaca, New York, on East Hill, offering views of the city and Cayuga Lake. The campus has expanded to approximately since its founding, now including multiple academic buildings, laboratories, administrative facilities, athletic centers, auditoriums, museums, and residential areas.

Geographic entities mentioned:
surface_form: Cayuga Lake
instance_of: Lake
countries: United States
coordinates: lat: 42.68805555555556
lon: -76.70222222222222
The architectural styles on the campus range from ornate Collegiate Gothic, Victorian, and Neoclassical buildings to more spare international and modernist structures. Frederick Law Olmsted, designer of Central Park, proposed a &quot;grand terrace&quot; overlooking Cayuga Lake in one of the earliest plans for the development of the campus.

Geographic entities mentioned:
surface_form: Cayuga Lake
instance_of: Lake
countries: United States
coordinates: lat: 42.68805555555556
lon: -76.70222222222222
Natural surroundings. Cornell University's main campus in Ithaca is located in the Finger Lakes region in upstate New York and features views of the city, Cayuga Lake, and surrounding valleys. The campus is bordered by two gorges, Fall Creek Gorge and Cascadilla Gorge.

Geographic entities mentioned:
surface_form: Finger Lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 42.666666666667
lon: -76.833333333333
surface_form: Cayuga Lake
instance_of: Lake
countries: United States
coordinates: lat: 42.68805555555556
lon: -76.70222222222222
Emerson Lake. Emerson Lake is a dry lake bed in the Mojave Desert of San Bernardino County, California, northeast of Joshua Tree. The lake is approximately long and at its widest point. Emerson Lake is on federal lands within the borders of the Marine Corps Air Ground Combat Center Twentynine Palms, west of Hildago Mountain.

Geographic entities mentioned:
surface_form: dry lake
instance_of: Lake
countries: United States
coordinates: lat: 44.6282988
lon: -97.0561783
surface_form: dry lake
instance_of: Lake
countries: United States
coordinates: lat: 38.3360373
lon: -117.7898285
surface_form: dry lake
instance_of: Lake
countries: United States
coordinates: lat: 45.0425
lon: -97.31972222
surface_form: emerson lake
instance_of: Lake
countries: United States
coordinates: lat: 34.4491
lon: -116.396
Emerson Lake. Emerson Lake is a dry lake bed in the Mojave Desert of San Bernardino County, California, northeast of Joshua Tree. The lake is approximately long and at its widest point. Emerson Lake is on federal lands within the borders of the Marine Corps Air Ground Combat Center Twentynine Palms, west of Hildago Mountain.

Geographic entities mentioned:
surface_form: emerson lake
instance_of: Lake
countries: United States
coordinates: lat: 34.4491
lon: -116.396
The park fills the west side of the &quot;X&quot; where the borders of Kazakhstan, Russia, China, and Mongolia meet. The highest peak in Siberia (Belukha Mountain,), is on the Russian border in the Katun Range. The park is in Katonkaragay District of East Kazakhstan Region, southeast of the capital city of Astana.

Geographic entities mentioned:
surface_form: Belukha Mountain
instance_of: Mountain
countries: Russia
Kazakhstan
Russian Empire
Soviet Union
coordinates: lat: 49.806944444444
lon: 86.589722222222
After the six-month rescue mission, Grande Island was rehabilitated and was restored to its Special Services resort configuration until 1991. At that time, the lease on US military bases expired, and the US bases were closed about the same time they were damaged by the eruption of Mount Pinatubo.

Geographic entities mentioned:
surface_form: Mount Pinatubo
instance_of: Mountain
countries: Philippines
coordinates: lat: 15.13
lon: 120.35
Lobstick Lake. Lobstick Lake became part of the Smallwood Reservoir, along with Michikamau Lake, upon the damming of the Churchill River in western Labrador, Newfoundland and Labrador, Canada. It forms the western section of the Smallwood Reservoir and lies just north of Ossokmanuan Lake. Fishing. The Lobstick Lake has a large population of lake trout.

Geographic entities mentioned:
surface_form: Michikamau Lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.1833
lon: -63.9992
surface_form: lobstick lake
instance_of: Lake
countries: Canada
coordinates: lat: 54
lon: -64.9992
Lobstick Lake. Lobstick Lake became part of the Smallwood Reservoir, along with Michikamau Lake, upon the damming of the Churchill River in western Labrador, Newfoundland and Labrador, Canada. It forms the western section of the Smallwood Reservoir and lies just north of Ossokmanuan Lake. Fishing. The Lobstick Lake has a large population of lake trout.

Geographic entities mentioned:
surface_form: lobstick lake
instance_of: Lake
countries: Canada
coordinates: lat: 54
lon: -64.9992
It forms the western section of the Smallwood Reservoir and lies just north of Ossokmanuan Lake. Fishing. The Lobstick Lake has a large population of lake trout. Fishermen and anglers frequently catch fish weighing five pounds, with some captured specimens being over 40 pounds.

Geographic entities mentioned:
surface_form: lobstick lake
instance_of: Lake
countries: Canada
coordinates: lat: 54
lon: -64.9992
His wife Marita Iversdatter Kleppo died in 1920. Rosemaling. Rosemaling means &quot;rose painting&quot;, and is a traditional Norwegian decorative painting style. Rosemaling in Norway originated in the low-land areas of eastern Norway particularly in Telemark and Hallingdal, but also in Numedal and Setesdal and in other valleys in Vest-Agder, Hordaland, Sogn og Fjordane and Rogaland.

Geographic entities mentioned:
surface_form: Hallingdal
instance_of: Valley
countries: Norway
coordinates: lat: 60.633333333333
lon: 9.05
surface_form: Numedal
instance_of: Valley
countries: Norway
coordinates: lat: 60
lon: 9.2
surface_form: Setesdal
instance_of: Valley
countries: Norway
coordinates: lat: 58.92025
lon: 7.7206388888889
Sierra Buttes. Sierra Buttes is an mountain summit located in the Sierra Nevada mountain range in Sierra County, California, United States. It is the third-highest point in Sierra County following the north ridge of Mount Lola and Peak 8740. Sierra Buttes are set on land managed by Tahoe National Forest and are within the North Yuba River watershed.

Geographic entities mentioned:
surface_form: Mount Lola
instance_of: Mountain
countries: United States
coordinates: lat: 39.4331
lon: -120.365
Topographic relief is significant as the southwest aspect rises nearly above the Yuba–Donner Scenic Byway in approximately two miles. The prominent fortress-like landform is visible from as far as the Sacramento Valley, and inclusion on the Sierra Peaks Section peakbagging list generates climbing interest. This landform's toponym has been officially adopted by the U.S.

Geographic entities mentioned:
surface_form: Sacramento Valley
instance_of: Valley
countries: United States
coordinates: lat: 39
lon: -121.5
surface_form: sacramento valley
instance_of: Valley
countries: United States
coordinates: lat: 34.8147
lon: -114.161
The hike to the lookout is one of the most popular destinations in the northern Sierra region. The Sierra Buttes trail is 2.3 miles long, gains 1,587 feet of elevation, and one mile of it is shared with the Pacific Crest Trail. In good weather, Lassen Peak can be seen from the lookout, 65 miles to the northwest, as well as Mount Shasta 150 miles distant. Sierra Valley can be seen to the east.

Geographic entities mentioned:
surface_form: Lassen Peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.488055555555555
lon: -121.505
surface_form: Mount Shasta
instance_of: Mountain
countries: United States
coordinates: lat: 41.409197222222
lon: -122.19488888889
surface_form: the lookout
instance_of: Mountain
countries: United States
coordinates: lat: 40.509444444444
lon: -75.346111111111
surface_form: shasta
instance_of: Mountain
countries: United States
coordinates: lat: 41.409197222222
lon: -122.19488888889
The Sierra Buttes trail is 2.3 miles long, gains 1,587 feet of elevation, and one mile of it is shared with the Pacific Crest Trail. In good weather, Lassen Peak can be seen from the lookout, 65 miles to the northwest, as well as Mount Shasta 150 miles distant. Sierra Valley can be seen to the east. Climate.

Geographic entities mentioned:
surface_form: Sierra Valley
instance_of: Valley
countries: United States
coordinates: lat: 39.77083333
lon: -120.32777778
Lookout. A fire lookout tower that was originally built in 1915 tops the highest point on Sierra Buttes. In 1964, employees of the National Forest Service erected metal stairs with railings for the public to safely access the views from the lookout. The hike to the lookout is one of the most popular destinations in the northern Sierra region.

Geographic entities mentioned:
surface_form: the lookout
instance_of: Mountain
countries: United States
coordinates: lat: 40.509444444444
lon: -75.346111111111
In 1964, employees of the National Forest Service erected metal stairs with railings for the public to safely access the views from the lookout. The hike to the lookout is one of the most popular destinations in the northern Sierra region. The Sierra Buttes trail is 2.3 miles long, gains 1,587 feet of elevation, and one mile of it is shared with the Pacific Crest Trail.

Geographic entities mentioned:
surface_form: the lookout
instance_of: Mountain
countries: United States
coordinates: lat: 40.509444444444
lon: -75.346111111111
Sierra Buttes. Sierra Buttes is an mountain summit located in the Sierra Nevada mountain range in Sierra County, California, United States. It is the third-highest point in Sierra County following the north ridge of Mount Lola and Peak 8740. Sierra Buttes are set on land managed by Tahoe National Forest and are within the North Yuba River watershed.

Geographic entities mentioned:
surface_form: sierra buttes
instance_of: Mountain
countries: United States
coordinates: lat: 39.5943
lon: -120.6477
It is the third-highest point in Sierra County following the north ridge of Mount Lola and Peak 8740. Sierra Buttes are set on land managed by Tahoe National Forest and are within the North Yuba River watershed. The summit is situated north of Sierra City, and approximately northeast of Sacramento.

Geographic entities mentioned:
surface_form: sierra buttes
instance_of: Mountain
countries: United States
coordinates: lat: 39.5943
lon: -120.6477
Board on Geographic Names, and has been in use since at least 1896 when published by the Sierra Club. Lookout. A fire lookout tower that was originally built in 1915 tops the highest point on Sierra Buttes. In 1964, employees of the National Forest Service erected metal stairs with railings for the public to safely access the views from the lookout.

Geographic entities mentioned:
surface_form: sierra buttes
instance_of: Mountain
countries: United States
coordinates: lat: 39.5943
lon: -120.6477
The hike to the lookout is one of the most popular destinations in the northern Sierra region. The Sierra Buttes trail is 2.3 miles long, gains 1,587 feet of elevation, and one mile of it is shared with the Pacific Crest Trail. In good weather, Lassen Peak can be seen from the lookout, 65 miles to the northwest, as well as Mount Shasta 150 miles distant. Sierra Valley can be seen to the east.

Geographic entities mentioned:
surface_form: sierra buttes
instance_of: Mountain
countries: United States
coordinates: lat: 39.5943
lon: -120.6477
In good weather, Lassen Peak can be seen from the lookout, 65 miles to the northwest, as well as Mount Shasta 150 miles distant. Sierra Valley can be seen to the east. Climate. According to the Köppen climate classification system, Sierra Buttes 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: sierra buttes
instance_of: Mountain
countries: United States
coordinates: lat: 39.5943
lon: -120.6477
Geology. The Sierra Buttes are composed of metavolcanic rock, predominantly andesitic hydroclastic breccia and peperite which intruded the Sierra Buttes Formation. The rock is part of the Northern Sierra Terrane and was formed in an undersea volcanic process along an island arc during the late Devonian period.

Geographic entities mentioned:
surface_form: sierra buttes
instance_of: Mountain
countries: United States
coordinates: lat: 39.5943
lon: -120.6477
surface_form: sierra buttes
instance_of: Mountain
countries: United States
coordinates: lat: 39.5943
lon: -120.6477
The rock is part of the Northern Sierra Terrane and was formed in an undersea volcanic process along an island arc during the late Devonian period. Gold nuggets were discovered at mines surrounding the Sierra Buttes during the California Gold Rush, the largest of which weighed 106 pounds was uncovered in 1869.

Geographic entities mentioned:
surface_form: sierra buttes
instance_of: Mountain
countries: United States
coordinates: lat: 39.5943
lon: -120.6477
Mount Dzebobo. Mount Dzebobo () is the second highest mountain in Ghana with a height of 876 meters. It is located in the Akwapim-Togo Range right on the border with Togo. The mountain is located just a few kilometres south of Kyabobo National Park.

Geographic entities mentioned:
surface_form: mount dzebobo
instance_of: Mountain
countries: Ghana
coordinates: lat: 8.33333333
lon: 0.6
surface_form: dzebobo
instance_of: Mountain
countries: Ghana
coordinates: lat: 8.33333333
lon: 0.6
After the old church was torn down in 1722, a new timber-framed church was built about to the northwest. The old church site was somewhat of a wetland area and it was prone to flooding. The new church sits near the mouth of the river Norddøla and the lake Holsavatnet. In 1861, the small timber-framed church was torn down and a new church was built on the same site.

Geographic entities mentioned:
surface_form: Holsavatnet
instance_of: Lake
countries: Norway
coordinates: lat: 61.416666666667
lon: 6.1
The trail continues into downtown Orting, paralleling (but not on) Washington State Route 162, and passing through the city's Central Park. There are frequent views of Mount Rainier during this short section. The path advances on to South Prairie while overlooking the Carbon River during certain stretches.

Geographic entities mentioned:
surface_form: Mount Rainier
instance_of: Mountain
countries: United States
coordinates: lat: 46.85166666666667
lon: -121.76027777777777
It lies in the Cordillera Real of Bolivia in the La Paz Department, Los Andes Province, Batallas Municipality, Kirani Canton. It is situated on the western side of the Janq'u Quta valley next to the mountains Warawarani and Phaq'u Kiwuta.

Geographic entities mentioned:
surface_form: Phaq'u Kiwuta
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.08805556
lon: -68.34555556
surface_form: phaq'u kiwuta
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.08805556
lon: -68.34555556
surface_form: warawarani
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.62194444
lon: -66.79055556
surface_form: warawarani
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.41361111
lon: -66.65972222
It is situated on the western side of the Janq'u Quta valley next to the mountains Warawarani and Phaq'u Kiwuta. Other prominent mountains nearby are Janq'u Laya and Janq'u Uyu in the north, and Wila Lluxita and Mullu Apachita in the northeast, all of them higher than 5,000 m.

Geographic entities mentioned:
surface_form: Janq'u Uyu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.05
lon: -68.32111111
surface_form: Wila Lluxita
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.0514
lon: -68.2969
surface_form: Mullu Apachita
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.0644
lon: -68.2889
surface_form: apachita
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.3061
lon: -69.4011
surface_form: apachita
instance_of: Mountain
countries: Bolivia
coordinates: lat: -22.4442
lon: -67.7911
surface_form: lluxita
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.70527778
lon: -66.86111111
surface_form: wila lluxita
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.0514
lon: -68.2969
surface_form: janq'u uyu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.05
lon: -68.32111111
surface_form: apachita
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.7631
lon: -68.5361
surface_form: mullu apachita
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.0644
lon: -68.2889
surface_form: lluxita
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.05833333
lon: -67.54722222
surface_form: apachita
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.465
lon: -67.12388889
surface_form: lluxita
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.75777778
lon: -65.72166667
Wila Lluxi. Wila Lluxi (Aymara &quot;wila&quot; blood, blood-red, &quot;lluxi&quot; shell of a mussel; landslide, &quot;red shell&quot; or &quot;red landslide&quot;, Hispanicized spellings &quot;Wila Lloje, Huilaroje&quot;) is a mountain in the Andes, about 5,596 m (18,360 ft) high.

Geographic entities mentioned:
surface_form: wila lloje
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.0747
lon: -68.3397
surface_form: wila lluxi
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.0747
lon: -68.3397
surface_form: huilaroje
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.0747
lon: -68.3397
Wila Lluxi. Wila Lluxi (Aymara &quot;wila&quot; blood, blood-red, &quot;lluxi&quot; shell of a mussel; landslide, &quot;red shell&quot; or &quot;red landslide&quot;, Hispanicized spellings &quot;Wila Lloje, Huilaroje&quot;) is a mountain in the Andes, about 5,596 m (18,360 ft) high.

Geographic entities mentioned:
surface_form: wila lluxi
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.0747
lon: -68.3397
Calaveras Valley. Calaveras Valley is a valley east of Milpitas, California in the San Francisco Bay Area. It has formed primarily as a result of the actions of the Calaveras Fault. The southern end of the Calaveras Valley is a few miles south of Calaveras Reservoir, while the northern end is at Sunol. &quot;See&quot; Calaveras Reservoir for more information.

Geographic entities mentioned:
surface_form: calaveras valley
instance_of: Valley
countries: United States
coordinates: lat: 37.4542
lon: -121.809
Taymouth Castle. Taymouth Castle is situated to the north-east of the village of Kenmore, Perth and Kinross, in the Highlands of Scotland, in an estate which encompasses. It lies on the south bank of the River Tay, about from Loch Tay, in the heartland of the Grampian Mountains.

Geographic entities mentioned:
surface_form: Loch Tay
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.515555555556
lon: -4.1461111111111
There were also some wild Indian buffaloes, taken from the 'rocky mountains of the New World'. Fly fishing. The castle offers of salmon fishing through the estate, on the River Tay. The estate also has fishing rights on Loch Tay, which contains pike, perch, roach and trout. The Campbells of Breadalbane and Glenorchy.

Geographic entities mentioned:
surface_form: Loch Tay
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.515555555556
lon: -4.1461111111111
In the usual way, the ownership of the estate (and the various titles) were generally passed from father to son, excepting when there were no male heirs. This particular branch of the Campbell family were given the titles of Breadalbane, an area in the Highlands of Scotland; and Glenorchy, a glen in Argyll and Bute. A number of the Campbells were Earls of Breadalbane and Holland.

Geographic entities mentioned:
surface_form: Glenorchy
instance_of: Valley
countries: United Kingdom
coordinates: lat: 56.48
lon: -4.82
It was declared by the company that they intended to convert the castle into a hydropathic hotel, along with opening a brand new golf course on its lands. The company also acquired fishing rights on Loch Tay and part of the River Tay and shooting rights on Drumhill. At the same time, there was a huge auction at the castle, in which all of its furniture and effects were sold.

Geographic entities mentioned:
surface_form: Loch Tay
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.515555555556
lon: -4.1461111111111
Early history of Balloch Castle. The landowners of Balloch Castle, together with dates of ownership and significant events are shown below:-
Sir Colin Campbell of Glenorchy (1550–1583). Sir Colin Campbell of Glenorchy, otherwise known as 'Grey Colin' because of his white hair and long flowing beard, became laird of Glenorchy upon the death of his older brother John, in 1550.

Geographic entities mentioned:
surface_form: Glenorchy
instance_of: Valley
countries: United Kingdom
coordinates: lat: 56.48
lon: -4.82
Despite this strategic victory, George Sinclair later won his argument in court in 1681 and claimed the title of Earl of Caithness and the lands. However, Campbell was compensated for the loss of these, by King Charles II and the Privy Council of Scotland elevating him to Lord of Glenorchy, Benederaloch, Ormelie and Wick, Viscount of Tay and Paintland, and 1st Earl of Breadalbane and Holland.

Geographic entities mentioned:
surface_form: Glenorchy
instance_of: Valley
countries: United Kingdom
coordinates: lat: 56.48
lon: -4.82
The following cities are members of the Gateway Cities Council of Governments, though these cities at times may also be considered part of other LA regions, including the San Gabriel Valley Region, East Los Angeles Region, the South Los Angeles Region, the Southeast LA (or SELA) region, and the Los Angeles Harbor Region. Air.

Geographic entities mentioned:
surface_form: San Gabriel Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.101944444444
lon: -118.10277777778
Woodbastwick. Woodbastwick () is a village and civil parish in the English county of Norfolk. It is located on the River Bure between Cockshoot Broad and Salhouse Broad, within The Broads and close to Bure Marshes NNR (national nature reserve). The city of Norwich lies to the south-west. The civil parish also includes the villages of Ranworth and Panxworth.

Geographic entities mentioned:
surface_form: Cockshoot Broad
instance_of: Lake
countries: United Kingdom
coordinates: lat: 52.695451
lon: 1.465939
surface_form: Salhouse Broad
instance_of: Lake
countries: United Kingdom
coordinates: lat: 52.689444444444
lon: 1.4294444444444
Agardhelva. Agardhelva is a river forming the border between Sabine Land and Heer Land at Spitsbergen, Svalbard. It flows through the valley of Agardhdalen, from the glaciers Elfenbeinbreen and Sveigbreen, ending into the bay Agardhbukta at the western side of Storfjorden. The river is named after botanist Jacob Georg Agardh.

Geographic entities mentioned:
surface_form: Agardhdalen
instance_of: Valley
countries: Norway
coordinates: lat: 78.09861111
lon: 18.27916667
Andrew's University. The &quot;Milton Loch 3&quot; site was discovered after investigation of a supposed island in the middle of the loch was surveyed. The crannog was built on the bedrock of the lake with some timbers being exposed. Like the other two crannogs, the timbers had been degraded by microorganisms. Using carbon dating, the site was dated to the late 5th century AD.

Geographic entities mentioned:
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
Milton Loch. Milton Loch is an alkaline freshwater loch located in Dumfries and Galloway, Scotland. In the loch and nearby are archaeological sites including three crannogs. Location. Milton Loch is in the region of Dumfries and Galloway and more locally, the parish of Urr. It is part of the Urr Basin. Close locations include Milton, Crocketford and Dumfries. Guido's excavations.

Geographic entities mentioned:
surface_form: milton loch
instance_of: Lake
countries: United Kingdom
coordinates: lat: 55.016666666667
lon: -3.8166666666667
Guido's excavations. In 1953, two separate crannogs were discovered in the loch after the water level was lowered. They were both excavated in 1955 by Peggy Guido (named C M Piggott in the excavation reports due to her marriage to Stuart Piggott). The first of the two sites, &quot;Milton Loch 1&quot;, is located in the northwest section of the loch. Excavations began in the autumn.

Geographic entities mentioned:
surface_form: milton loch
instance_of: Lake
countries: United Kingdom
coordinates: lat: 55.016666666667
lon: -3.8166666666667
Artifacts retrieved from the site include a fish-club, plough-head, bronze dress-fastener, mallet-head and two slotted planks; some of the artifacts are in the care of Dumfries Museum. The second of the two sites, &quot;Milton Loch 2&quot;, is located in the southeast section of the loch. Guido discovered it due to some timbers exposed above the water level.

Geographic entities mentioned:
surface_form: milton loch
instance_of: Lake
countries: United Kingdom
coordinates: lat: 55.016666666667
lon: -3.8166666666667
The crannog was built on the bedrock of the lake with some timbers being exposed. Like the other two crannogs, the timbers had been degraded by microorganisms. Using carbon dating, the site was dated to the late 5th century AD. Dixon also noted another site on the same outcrop, named &quot;Milton Loch 4&quot;. Suspected again to be a crannog, it turned out to be an island in the loch.

Geographic entities mentioned:
surface_form: milton loch
instance_of: Lake
countries: United Kingdom
coordinates: lat: 55.016666666667
lon: -3.8166666666667
Outnumbered, the SS guards moved out, leaving the prisoners behind. The prisoners were then set free, with the majority opting for sanctuary for a time in Pragser Wildsee under the protection of Alvensleben's troops until a U.S. force arrived to take custody. After the war. In autumn 1945, Alvensleben was released from U.S.

Geographic entities mentioned:
surface_form: Pragser Wildsee
instance_of: Lake
countries: Italy
coordinates: lat: 46.69361111111111
lon: 12.085
Kutschenberg. The Kutschenberg is the highest hill in Brandenburg, Germany. It is part of the low hill range of the Kmehlener Berge and rises near Großkmehlen in the county of Oberspreewald-Lausitz. It is and located only a few metres from the state border with Saxony. Location.

Geographic entities mentioned:
surface_form: Kmehlener Berge
instance_of: Mountain
countries: Germany
coordinates: lat: 51.3667
lon: 13.7333
There is commonly held notion that the Hagelberg (200.24 m) on the Fläming Heath is the highest hill in Brandenburg, but the Kutschenberg is just a little higher. Am Kutschenberg racetrack. On the northeast hillside of the Kutschenberg about 400 metres from the summit is the nationally known offroad racetrack of &quot;Am Kutschenberg&quot;, where car and motorcycle races are regularly held.

Geographic entities mentioned:
surface_form: Hagelberg
instance_of: Mountain
countries: Germany
coordinates: lat: 52.1386
lon: 12.5172
surface_form: hagelberg
instance_of: Mountain
countries: Germany
coordinates: lat: 52.1386
lon: 12.5172
surface_form: kutschenberg
instance_of: Mountain
countries: Germany
coordinates: lat: 51.3653
lon: 13.7272
surface_form: kutschenberg
instance_of: Mountain
countries: Germany
coordinates: lat: 51.3653
lon: 13.7272
Kutschenberg. The Kutschenberg is the highest hill in Brandenburg, Germany. It is part of the low hill range of the Kmehlener Berge and rises near Großkmehlen in the county of Oberspreewald-Lausitz. It is and located only a few metres from the state border with Saxony. Location.

Geographic entities mentioned:
surface_form: kutschenberg
instance_of: Mountain
countries: Germany
coordinates: lat: 51.3653
lon: 13.7272
It is and located only a few metres from the state border with Saxony. Location. The Kutschenberg is 2.5 km west-southwest of Ortrand and 1.5 kilometres south of Großkmehlen not far from the A 13 motorway to the west and within a small area of woodland in the Kmehlener Berge. Height.

Geographic entities mentioned:
surface_form: kutschenberg
instance_of: Mountain
countries: Germany
coordinates: lat: 51.3653
lon: 13.7272
surface_form: kmehlener berge
instance_of: Mountain
countries: Germany
coordinates: lat: 51.3667
lon: 13.7333
Height. New surveys in 2000 discovered that the summit of the Kutschenberg was 201.0 m high and thus the highest hill in the state of Brandenburg. As a result, in 2011 a small granite stele was erected on its densely wooded summit that rises only slightly above its surroundings. The stele is inscribed with the words &quot;KUTSCHENBERG 201 m ü. NHN&quot;. Near the summit at 199.7 m is a trig point.

Geographic entities mentioned:
surface_form: kutschenberg
instance_of: Mountain
countries: Germany
coordinates: lat: 51.3653
lon: 13.7272
The stele is inscribed with the words &quot;KUTSCHENBERG 201 m ü. NHN&quot;. Near the summit at 199.7 m is a trig point. About 11 km to the west near Gröden is the Heidehöhe which, at 201.4 m, is slightly higher than the Kutschenberg, but is not the highest hill in Brandenburg, but its highest point, because the summit above it, the &quot;Heideberg&quot;, lies in Saxony.

Geographic entities mentioned:
surface_form: kutschenberg
instance_of: Mountain
countries: Germany
coordinates: lat: 51.3653
lon: 13.7272
surface_form: heideberg
instance_of: Mountain
countries: Germany
coordinates: lat: 53.8778
lon: 11.2847
There is commonly held notion that the Hagelberg (200.24 m) on the Fläming Heath is the highest hill in Brandenburg, but the Kutschenberg is just a little higher. Am Kutschenberg racetrack. On the northeast hillside of the Kutschenberg about 400 metres from the summit is the nationally known offroad racetrack of &quot;Am Kutschenberg&quot;, where car and motorcycle races are regularly held.

Geographic entities mentioned:
surface_form: kutschenberg
instance_of: Mountain
countries: Germany
coordinates: lat: 51.3653
lon: 13.7272
surface_form: kutschenberg
instance_of: Mountain
countries: Germany
coordinates: lat: 51.3653
lon: 13.7272
Life and politics. Duncan was born in Lyons, New York on May 18, 1820. The family moved to Rochester, New York in 1825, and in 1841 Duncan began working as a steward on the passenger steamers crossing the Great Lakes. In 1846, he changed employers and began working on a steamer traveling through Lake Superior. In 1849, Duncan moved to Detroit and became a brewer.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
Signhildsberg. Signhildsberg (historically Fornsigtuna, where &quot;forn&quot; means &quot;ancient&quot;, Old Sigtuna, &quot;Sithun&quot;, &quot;Signesberg&quot;) is a manor that formerly was a royal estate (Uppsala öd), located in the parish of Håtuna approximately west of the modern town of Sigtuna, by Lake Mälaren in Sweden.

Geographic entities mentioned:
surface_form: Mälaren
instance_of: Lake
countries: Sweden
coordinates: lat: 59.5
lon: 17.2
The EastAfrican. &quot;The EastAfrican&quot; is a weekly newspaper published in Kenya since 7 November 1994, by the Nation Media Group, which also publishes Kenya's national &quot;Daily Nation&quot;. The &quot;EastAfrican&quot; also circulates in the other countries of the African Great Lakes region, including Tanzania, Uganda, and Rwanda.

Geographic entities mentioned:
surface_form: African Great Lakes
instance_of: Group of lakes
countries: Burundi
Zambia
Kenya
Democratic Republic of the Congo
Malawi
Mozambique
Rwanda
Tanzania
Uganda
Ethiopia
coordinates: lat: -8
lon: 35