Sarmila/GeoWiki-Features huggingface dataset:
Selibüel. The Selibüel is a mountain of the Bernese Alpine foothills, located in the municipality of Rüschegg in the canton of Bern. It is the culminating point of the wooded range that lies north of the Gurnigel Pass, between the valleys of the Sense (west) and the Aare (east).

Geographic entities mentioned:
surface_form: Gurnigel Pass
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.7334
lon: 7.45277
surface_form: sense
instance_of: Watercourse
countries: Switzerland
coordinates: lat: 46.906
lon: 7.23389
It is the culminating point of the wooded range that lies north of the Gurnigel Pass, between the valleys of the Sense (west) and the Aare (east). The summit area, as well as the other summits of the range, such as the Pfyffe, is easily accessible by car or by bus via the Gurnigel road.

Geographic entities mentioned:
surface_form: Pfyffe
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.7422
lon: 7.372
surface_form: gurnigel
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.7334
lon: 7.45277
Selibüel. The Selibüel is a mountain of the Bernese Alpine foothills, located in the municipality of Rüschegg in the canton of Bern. It is the culminating point of the wooded range that lies north of the Gurnigel Pass, between the valleys of the Sense (west) and the Aare (east).

Geographic entities mentioned:
surface_form: selibüel
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.7334
lon: 7.45277
surface_form: selibüel
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.73166667
lon: 7.43861111
Haplochromis igneopinnis. &quot;Haplochromis igneopinnis&quot; is a species of cichlid endemic to the Tanzanian portion of Lake Victoria in the Speke Gulf. This species can reach a length of SL.

Geographic entities mentioned:
surface_form: Lake Victoria
instance_of: Lake
countries: Tanzania
Uganda
Kenya
coordinates: lat: -1
lon: 33
She later moved her school to Epping, changing the name of her school from the Epping Ladies' College to Osborne Ladies' College, in honour of the Royal Naval College, Osborne, on the Isle of Wight. In 1923 Gibbins moved her school to its final location on near Blackhheath overlooking the Kanimbla and Megalong Valleys. The building was the former site of an unused hotel built in 1888.

Geographic entities mentioned:
surface_form: Megalong Valley
instance_of: Valley
countries: Australia
coordinates: lat: -33.733333333333
lon: 150.25
Yunnan Nationalities Museum. The Yunnan Nationalities Museum () is located on the east bank of Dian Lake in Kunming, Yunnan, China, next to the Yunnan Ethnic Village. Opened on 9 November 1995, it is a comprehensive ethnology museum. Covering an area of over 200 mu, the museum has a building area of. It consists of various exhibition halls, office building, report hall, storage and workshops.

Geographic entities mentioned:
surface_form: Dian Lake
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 24.800555555556
lon: 102.67138888889
Dense forests, which supported a population of several thousand indigenous Aetas, heavily eroded and obscured Pinatubo. Pinatubo is known for its VEI-6 eruption on June 15, 1991, the second-largest terrestrial eruption of the 20th century after the 1912 eruption of Novarupta in Alaska.

Geographic entities mentioned:
surface_form: Novarupta
instance_of: Mountain
countries: United States
coordinates: lat: 58.266666666667
lon: -155.15666666667
surface_form: pinatubo
instance_of: Mountain
countries: Philippines
coordinates: lat: 15.13
lon: 120.35
It is part of a chain of volcanoes which lie along the western side of the island of Luzon called the Zambales Mountains. Pinatubo belongs to the Cabusilan sub-range of the Zambales Mountains, which consists of Mount Cuadrado, Mount Negron, Mount Mataba and Mount Pinatubo.

Geographic entities mentioned:
surface_form: Mount Cuadrado
instance_of: Mountain
countries: Philippines
coordinates: lat: 15.032222222222
lon: 120.34666666667
surface_form: Mount Negron
instance_of: Mountain
countries: Philippines
coordinates: lat: 15.094166666667
lon: 120.36722222222
surface_form: pinatubo
instance_of: Mountain
countries: Philippines
coordinates: lat: 15.13
lon: 120.35
surface_form: pinatubo
instance_of: Mountain
countries: Philippines
coordinates: lat: 15.13
lon: 120.35
surface_form: mount pinatubo
instance_of: Mountain
countries: Philippines
coordinates: lat: 15.13
lon: 120.35
The mountain was soon turned into the abode of Apo Namalyari (&quot;The lord of happenings/events&quot;), the pagan deity of the Sambal, Aetas and Kapampangans living on the Zambales range. It was said to comprise the whole mountain range until Sinukuan of Mount Arayat (the god of the Kapampangans) became a strong rival of Namalyari.

Geographic entities mentioned:
surface_form: Mount Arayat
instance_of: Mountain
countries: Philippines
coordinates: lat: 15.2
lon: 120.742
surface_form: mount arayat
instance_of: Mountain
countries: Philippines
coordinates: lat: 15.2
lon: 120.742
surface_form: arayat
instance_of: Mountain
countries: Philippines
coordinates: lat: 15.2
lon: 120.742
Pinatubo&quot;. The plane crashed into Mount Manunggal in Cebu province in 1957, killing the president and twenty-four others on board. The shape of Mount Pinatubo's caldera inspired New Clark City Athletics Stadium in Capas, Tarlac. Hiking activity.

Geographic entities mentioned:
surface_form: Mount Manunggal
instance_of: Mountain
countries: Philippines
coordinates: lat: 10.453055555555556
lon: 123.815
Several mountains near modern Pinatubo are old satellite vents of ancestral Pinatubo, forming volcanic plugs and lava domes. These satellite vents were probably active around the same time as the ancestral volcano and include the domes of Mount Negron, Mount Cuadrado, Mount Mataba and the Bituin and Tapungho plugs. Modern Pinatubo.

Geographic entities mentioned:
surface_form: mount negron
instance_of: Mountain
countries: Philippines
coordinates: lat: 15.094166666667
lon: 120.36722222222
surface_form: mount cuadrado
instance_of: Mountain
countries: Philippines
coordinates: lat: 15.032222222222
lon: 120.34666666667
Mount Pinatubo. Mount Pinatubo is an active stratovolcano in the Zambales Mountains in Luzon in the Philippines. Located on the tripoint of Zambales, Tarlac and Pampanga provinces, most people were unaware of its eruptive history before the pre-eruption volcanic activity in early 1991.

Geographic entities mentioned:
surface_form: pinatubo
instance_of: Mountain
countries: Philippines
coordinates: lat: 15.13
lon: 120.35
surface_form: mount pinatubo
instance_of: Mountain
countries: Philippines
coordinates: lat: 15.13
lon: 120.35
Mount Pinatubo is an active stratovolcano in the Zambales Mountains in Luzon in the Philippines. Located on the tripoint of Zambales, Tarlac and Pampanga provinces, most people were unaware of its eruptive history before the pre-eruption volcanic activity in early 1991. Dense forests, which supported a population of several thousand indigenous Aetas, heavily eroded and obscured Pinatubo.

Geographic entities mentioned:
surface_form: pinatubo
instance_of: Mountain
countries: Philippines
coordinates: lat: 15.13
lon: 120.35
Geography. The volcano is about northwest of Manila, the capital of the Philippines. Near Mount Pinatubo are former military bases that were maintained by the United States. The U.S. Naval Base Subic Bay was south of Pinatubo, and the extent of Clark Air Base was just east of the volcano's summit. The volcano is near to about 6 million people. History.

Geographic entities mentioned:
surface_form: pinatubo
instance_of: Mountain
countries: Philippines
coordinates: lat: 15.13
lon: 120.35
surface_form: mount pinatubo
instance_of: Mountain
countries: Philippines
coordinates: lat: 15.13
lon: 120.35
Geography. The volcano is about northwest of Manila, the capital of the Philippines. Near Mount Pinatubo are former military bases that were maintained by the United States. The U.S. Naval Base Subic Bay was south of Pinatubo, and the extent of Clark Air Base was just east of the volcano's summit. The volcano is near to about 6 million people. History.

Geographic entities mentioned:
surface_form: pinatubo
instance_of: Mountain
countries: Philippines
coordinates: lat: 15.13
lon: 120.35
The volcano is near to about 6 million people. History. Even before the 1991 eruption, Mount Pinatubo had little topographic prominence: it was above sea level, only about above nearby plains, and only about higher than surrounding peaks, which largely obscured it from view. It is part of a chain of volcanoes which lie along the western side of the island of Luzon called the Zambales Mountains.

Geographic entities mentioned:
surface_form: pinatubo
instance_of: Mountain
countries: Philippines
coordinates: lat: 15.13
lon: 120.35
surface_form: mount pinatubo
instance_of: Mountain
countries: Philippines
coordinates: lat: 15.13
lon: 120.35
They are subduction volcanoes, formed by the Eurasian plate sliding under the Philippine Mobile Belt along the Manila Trench to the west. Mount Pinatubo and the other volcanoes on this volcanic belt arise due to magmatic occlusion from this subduction plate boundary.

Geographic entities mentioned:
surface_form: pinatubo
instance_of: Mountain
countries: Philippines
coordinates: lat: 15.13
lon: 120.35
surface_form: mount pinatubo
instance_of: Mountain
countries: Philippines
coordinates: lat: 15.13
lon: 120.35
Mount Pinatubo and the other volcanoes on this volcanic belt arise due to magmatic occlusion from this subduction plate boundary. Pinatubo is flanked on the west by the Zambales Ophiolite Complex, which is an easterly-dipping section of Eocene oceanic crust uplifted during the late Oligocene.

Geographic entities mentioned:
surface_form: pinatubo
instance_of: Mountain
countries: Philippines
coordinates: lat: 15.13
lon: 120.35
Pinatubo is flanked on the west by the Zambales Ophiolite Complex, which is an easterly-dipping section of Eocene oceanic crust uplifted during the late Oligocene. The Tarlac Formation north, east and southeast of Pinatubo consists of marine, nonmarine and volcanoclastic sediments formed in the late Miocene and Pliocene.

Geographic entities mentioned:
surface_form: pinatubo
instance_of: Mountain
countries: Philippines
coordinates: lat: 15.13
lon: 120.35
The Tarlac Formation north, east and southeast of Pinatubo consists of marine, nonmarine and volcanoclastic sediments formed in the late Miocene and Pliocene. The most recent study of Mount Pinatubo before the activities of 1991 was the overall geological study in 1983 and 1984 made by F. G.

Geographic entities mentioned:
surface_form: pinatubo
instance_of: Mountain
countries: Philippines
coordinates: lat: 15.13
lon: 120.35
surface_form: mount pinatubo
instance_of: Mountain
countries: Philippines
coordinates: lat: 15.13
lon: 120.35
G. Delfin for the Philippine National Oil Company as part of the surface investigations of the area before exploratory drilling and well testing for geothermal energy sources in 1988 to 1990. He recognized two life histories of the mountain, which he classified as &quot;ancestral&quot; and &quot;modern&quot; Pinatubo. Ancestral Pinatubo.

Geographic entities mentioned:
surface_form: pinatubo
instance_of: Mountain
countries: Philippines
coordinates: lat: 15.13
lon: 120.35
surface_form: pinatubo
instance_of: Mountain
countries: Philippines
coordinates: lat: 15.13
lon: 120.35
Ancestral Pinatubo. Activity of Ancestral Pinatubo seems to have begun about 1.1 million years ago and probably ended tens of thousands of years or more before the birth of &quot;modern&quot; Pinatubo. Much of the rugged land around the present volcano consists of remnants of &quot;ancestral&quot; Pinatubo.

Geographic entities mentioned:
surface_form: pinatubo
instance_of: Mountain
countries: Philippines
coordinates: lat: 15.13
lon: 120.35
surface_form: pinatubo
instance_of: Mountain
countries: Philippines
coordinates: lat: 15.13
lon: 120.35
Ancestral Pinatubo. Activity of Ancestral Pinatubo seems to have begun about 1.1 million years ago and probably ended tens of thousands of years or more before the birth of &quot;modern&quot; Pinatubo. Much of the rugged land around the present volcano consists of remnants of &quot;ancestral&quot; Pinatubo.

Geographic entities mentioned:
surface_form: pinatubo
instance_of: Mountain
countries: Philippines
coordinates: lat: 15.13
lon: 120.35
Much of the rugged land around the present volcano consists of remnants of &quot;ancestral&quot; Pinatubo. It was an andesite and dacite stratovolcano whose eruptive activity was much less explosive than modern Pinatubo. Its center was roughly where the current volcano is.

Geographic entities mentioned:
surface_form: pinatubo
instance_of: Mountain
countries: Philippines
coordinates: lat: 15.13
lon: 120.35
The old volcano is exposed in the walls of an old wide caldera, referred to as &quot;Tayawan Caldera&quot; by Delfin. Some of the nearby peaks are the remnants of ancestral Pinatubo, left behind when the softer parts of the old mountain slopes were eroded by weathering. Ancestral Pinatubo is a somma volcano with modern Pinatubo as the new cone.

Geographic entities mentioned:
surface_form: pinatubo
instance_of: Mountain
countries: Philippines
coordinates: lat: 15.13
lon: 120.35
surface_form: pinatubo
instance_of: Mountain
countries: Philippines
coordinates: lat: 15.13
lon: 120.35
Some of the nearby peaks are the remnants of ancestral Pinatubo, left behind when the softer parts of the old mountain slopes were eroded by weathering. Ancestral Pinatubo is a somma volcano with modern Pinatubo as the new cone. Mount Dorst, to the east, is part of the dip slope of the ancestral Pinatubo.

Geographic entities mentioned:
surface_form: pinatubo
instance_of: Mountain
countries: Philippines
coordinates: lat: 15.13
lon: 120.35
Ancestral Pinatubo is a somma volcano with modern Pinatubo as the new cone. Mount Dorst, to the east, is part of the dip slope of the ancestral Pinatubo. Several mountains near modern Pinatubo are old satellite vents of ancestral Pinatubo, forming volcanic plugs and lava domes.

Geographic entities mentioned:
surface_form: pinatubo
instance_of: Mountain
countries: Philippines
coordinates: lat: 15.13
lon: 120.35
surface_form: pinatubo
instance_of: Mountain
countries: Philippines
coordinates: lat: 15.13
lon: 120.35
Mount Dorst, to the east, is part of the dip slope of the ancestral Pinatubo. Several mountains near modern Pinatubo are old satellite vents of ancestral Pinatubo, forming volcanic plugs and lava domes. These satellite vents were probably active around the same time as the ancestral volcano and include the domes of Mount Negron, Mount Cuadrado, Mount Mataba and the Bituin and Tapungho plugs.

Geographic entities mentioned:
surface_form: pinatubo
instance_of: Mountain
countries: Philippines
coordinates: lat: 15.13
lon: 120.35
Some eruptive periods have lasted decades and perhaps as much as several centuries and might appear to include multiple large explosive eruptions. The maximum size of eruptions in each eruptive period though has been getting smaller through the more than 35,000-year history of modern Pinatubo, but this might be an artifact of erosion and burial of older deposits.

Geographic entities mentioned:
surface_form: pinatubo
instance_of: Mountain
countries: Philippines
coordinates: lat: 15.13
lon: 120.35
surface_form: pinatubo
instance_of: Mountain
countries: Philippines
coordinates: lat: 15.13
lon: 120.35
Fourteen hours later, a 15-minute blast hurled volcanic matter to heights of. Friction in the up-rushing ash column generated abundant volcanic lightning. In March and April 1991, magma rising toward the surface from more than beneath Pinatubo triggered small volcano tectonic earthquakes and caused powerful steam explosions that blasted three craters on the north flank of the volcano.

Geographic entities mentioned:
surface_form: pinatubo
instance_of: Mountain
countries: Philippines
coordinates: lat: 15.13
lon: 120.35
surface_form: pinatubo
instance_of: Mountain
countries: Philippines
coordinates: lat: 15.13
lon: 120.35
Thousands of small earthquakes occurred beneath Pinatubo through April, May and early June and many thousand of tons of noxious sulfur dioxide gas were also emitted by the volcano. From June 7 to 12, the first magma reached the surface of Mount Pinatubo.

Geographic entities mentioned:
surface_form: pinatubo
instance_of: Mountain
countries: Philippines
coordinates: lat: 15.13
lon: 120.35
surface_form: mount pinatubo
instance_of: Mountain
countries: Philippines
coordinates: lat: 15.13
lon: 120.35
Fine ash fell as far away as the Indian Ocean and satellites tracked the ash cloud several times around the globe. Huge pyroclastic flows roared down the flanks of Mount Pinatubo, filling once-deep valleys with fresh volcanic deposits as much as thick. The eruption removed so much magma and rock from below the volcano that the summit collapsed to form a wide caldera.

Geographic entities mentioned:
surface_form: pinatubo
instance_of: Mountain
countries: Philippines
coordinates: lat: 15.13
lon: 120.35
Volcanologists suspected that further violent eruptions could be possible, and some areas were evacuated. However, the eruption was only minor. The last eruption of Mount Pinatubo took place in 1993. Lake Pinatubo. The 1991 caldera afterwards filled with water from annual monsoon rains and a crater lake, Lake Pinatubo, was formed.

Geographic entities mentioned:
surface_form: pinatubo
instance_of: Mountain
countries: Philippines
coordinates: lat: 15.13
lon: 120.35
The last eruption of Mount Pinatubo took place in 1993. Lake Pinatubo. The 1991 caldera afterwards filled with water from annual monsoon rains and a crater lake, Lake Pinatubo, was formed. In 1992, a growing lava dome formed an island, which was eventually submerged by the lake. Initially, the lake was hot and highly acidic, with a minimum pH of 2 and a temperature of about.

Geographic entities mentioned:
surface_form: pinatubo
instance_of: Mountain
countries: Philippines
coordinates: lat: 15.13
lon: 120.35
Workers cut a notch in the crater rim and drained about a quarter of the lake's volume. Recent activity. On July 10, 2002, the west wall of the crater collapsed, slowly releasing approximately of water and sediment into the Maraunot River in Botolan, Zambales. On July 26, 2011, a 5.9 magnitude earthquake struck close to Pinatubo; however, no major damages or casualties were reported.

Geographic entities mentioned:
surface_form: pinatubo
instance_of: Mountain
countries: Philippines
coordinates: lat: 15.13
lon: 120.35
On July 26, 2011, a 5.9 magnitude earthquake struck close to Pinatubo; however, no major damages or casualties were reported. On March 4, 2021, the PHIVOLCS raised alert level 1 over Mount Pinatubo after reporting an increase on its seismic activity. 1,722 volcanic earthquakes were also recorded within the vicinity of the volcano since January 2021. On August 11, 2021, PHIVOLCS downgraded Mt.

Geographic entities mentioned:
surface_form: pinatubo
instance_of: Mountain
countries: Philippines
coordinates: lat: 15.13
lon: 120.35
surface_form: mount pinatubo
instance_of: Mountain
countries: Philippines
coordinates: lat: 15.13
lon: 120.35
PHIVOLCS said it noted a &quot;significant decrease&quot; in volcanic earthquakes, with a total of 104 quakes or an average 2–3 events per day recorded from July 1 – August 1, 2021. On November 30, 2021, PHIVOLCS reported a weak explosion occurred on Mt. Pinatubo between 12:09 p.m. and 12:13 p.m., which produced a plume.

Geographic entities mentioned:
surface_form: pinatubo
instance_of: Mountain
countries: Philippines
coordinates: lat: 15.13
lon: 120.35
After being driven away by the 1991 eruption of Mount Pinatubo, in May 2009 some 454 Aeta families in Pampanga were given the first clean ancestral land ownership on Mount Pinatubo with the Certificate of Ancestral Domain Title (CADT) by the National Commission on Indigenous Peoples (NCIP), the government agency that deals with issues concerning indigenous people of the Philippines.

Geographic entities mentioned:
surface_form: pinatubo
instance_of: Mountain
countries: Philippines
coordinates: lat: 15.13
lon: 120.35
surface_form: mount pinatubo
instance_of: Mountain
countries: Philippines
coordinates: lat: 15.13
lon: 120.35
On January 14, 2010, some 7,000 Aeta families from Zambales were officially granted the Certificate of Ancestral Domain Title (CADT) covering the Zambales side of Pinatubo which includes the summit and Lake Pinatubo, officially becoming their &quot;lutan tua&quot; (ancestral land).

Geographic entities mentioned:
surface_form: pinatubo
instance_of: Mountain
countries: Philippines
coordinates: lat: 15.13
lon: 120.35
surface_form: pinatubo
instance_of: Mountain
countries: Philippines
coordinates: lat: 15.13
lon: 120.35
Having the land title will protect them from others – including foreigners – exploiting their land without compensation to and consent from the indigenous tribes. In the past, the Aetas had to contend with mining companies, loggers, and recently, tourist companies who earn from Mount Pinatubo but do not compensate the local tribes. In popular culture.

Geographic entities mentioned:
surface_form: pinatubo
instance_of: Mountain
countries: Philippines
coordinates: lat: 15.13
lon: 120.35
surface_form: mount pinatubo
instance_of: Mountain
countries: Philippines
coordinates: lat: 15.13
lon: 120.35
In the past, the Aetas had to contend with mining companies, loggers, and recently, tourist companies who earn from Mount Pinatubo but do not compensate the local tribes. In popular culture. Long before Mount Pinatubo became famous for its cataclysmic eruption, Philippine president Ramon Magsaysay, a native of Zambales, named his C-47 presidential plane &quot;Mt. Pinatubo&quot;.

Geographic entities mentioned:
surface_form: pinatubo
instance_of: Mountain
countries: Philippines
coordinates: lat: 15.13
lon: 120.35
surface_form: mount pinatubo
instance_of: Mountain
countries: Philippines
coordinates: lat: 15.13
lon: 120.35
Pinatubo&quot;. The plane crashed into Mount Manunggal in Cebu province in 1957, killing the president and twenty-four others on board. The shape of Mount Pinatubo's caldera inspired New Clark City Athletics Stadium in Capas, Tarlac. Hiking activity.

Geographic entities mentioned:
surface_form: pinatubo
instance_of: Mountain
countries: Philippines
coordinates: lat: 15.13
lon: 120.35
The shape of Mount Pinatubo's caldera inspired New Clark City Athletics Stadium in Capas, Tarlac. Hiking activity. The caldera formed and Lake Pinatubo has, since June 15, 1991, become a tourist attraction with the preferred route through Barangay Santa Juliana in Capas, Tarlac. Mammals. The Long-nosed forest mouse (Apomys sacobianus) is a species of rodent endemic to Mount Pinatubo, Philippines.

Geographic entities mentioned:
surface_form: pinatubo
instance_of: Mountain
countries: Philippines
coordinates: lat: 15.13
lon: 120.35
Rapidly weakening, both the JTWC and JMA stopped tracking Herbert the next day. As Herbert made its closest approach to Hong Kong, some stations recorded moderate gales, with Tate's Cairn recording a gust of. Additionally, heavy rainfall was seen, flooding some roads and causing landslides. Two men died after their helicopter crashed into the slopes of Tai Mo Shan.

Geographic entities mentioned:
surface_form: Tate's Cairn
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 22.358
lon: 114.218
As Herbert made its closest approach to Hong Kong, some stations recorded moderate gales, with Tate's Cairn recording a gust of. Additionally, heavy rainfall was seen, flooding some roads and causing landslides. Two men died after their helicopter crashed into the slopes of Tai Mo Shan. The Paracel Islands recorded peak winds of. Typhoon Ida (Lusing).

Geographic entities mentioned:
surface_form: Tai Mo Shan
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 22.4118
lon: 114.123
The karst landscape where the fish was found covers around, making it the largest contiguous karst area in the country. From the location where &quot;O. caeca&quot; specimens were found, the karst landscape reaches Lake Kutubu, which is northwest. There is some oil and gas drilling in this area. The creek was about above sea level. Taxonomy.

Geographic entities mentioned:
surface_form: Lake Kutubu
instance_of: Lake
countries: Papua New Guinea
coordinates: lat: -6.4
lon: 143.33333333333
Alpine climber. Minnigerode was an Alpine climber and a member of the Basel section of the Swiss Alpine Club. One of the couloirs on the East face of the Ortler was named after Minnigerode following his first attempted climb in 1878. For further details of Minnigerode's climbing achievements see. Honours.

Geographic entities mentioned:
surface_form: Ortler
instance_of: Mountain
countries: Italy
coordinates: lat: 46.508888888889
lon: 10.545
Individuals weighing up to have been reported. The largest specimens were found in Bosnia and Herzegovina, inhabiting the Neretva River from below town of Konjic downstream to town of Čapljina, mostly in canyon section from town of Jablanica to city of Mostar, and later after construction of Jablanica Dam on the Neretva River in Jablaničko Lake.

Geographic entities mentioned:
surface_form: Jablaničko Lake
instance_of: Lake
countries: Bosnia and Herzegovina
coordinates: lat: 43.692222222222
lon: 17.8275
Like the &quot;Ḥanīf&quot;, Muhammad practiced &quot;Taḥannuth&quot;, spending time in seclusion at Mount Hira and &quot;turning away from paganism.&quot; When he was about 40 years old, he began receiving at mount Hira' what Muslims regard as divine revelations delivered through the angel Gabriel, which would later form the Quran.

Geographic entities mentioned:
surface_form: Mount Hira
instance_of: Mountain
countries: Saudi Arabia
coordinates: lat: 21.458055555556
lon: 39.861388888889
By the early 17th century, the descendants of their founders controlled much of the Muslim world, stretching from the Balkans and North Africa to the Bay of Bengal, with a combined population estimated at between 130 and 160 million. The empires all benefited from alliances between rulers and religious officials.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
It is owned by Nexstar Media Group alongside ABC affiliate WIVT (channel 34). The two stations share studios on Ingraham Hill Road in the town of Binghamton, where WBGH-CD's transmitter is also located. Even though WBGH-CD transmits a digital signal of its own, its broadcast range is limited to the immediate Binghamton area.

Geographic entities mentioned:
surface_form: Ingraham Hill
instance_of: Mountain
countries: United States
coordinates: lat: 42.0618
lon: -75.9511
Clair Avenue West. The eastern boundary followed Lansdowne all the way to Queen Street West, where it went eastward for a block, then went down the western side of Dunn Avenue to Lake Ontario. The western boundary started at the eastern side of Keele Street (since 1921, this part of Keele Street is named Parkside Drive) at Queen Street West (since 1956, this is called The Queensway).

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
Blue Lake (Hubbard County, Minnesota). Blue Lake is a lake in Hubbard County, in the U.S. state of Minnesota. Blue Lake was so named on account of the blueish tint of its waters.

Geographic entities mentioned:
surface_form: blue lake
instance_of: Lake
countries: United States
coordinates: lat: 27.4354
lon: -81.5117
surface_form: blue lake
instance_of: Lake
countries: United States
coordinates: lat: 41.1635044
lon: -74.2603249
surface_form: blue lake
instance_of: Lake
countries: United States
coordinates: lat: 46.1666
lon: -86.6321
surface_form: blue lake
instance_of: Lake
countries: United States
coordinates: lat: 47.415277777778
lon: -121.51861111111
surface_form: blue lake
instance_of: Lake
countries: United States
coordinates: lat: 40.501944444444
lon: -114.03222222222
surface_form: blue lake
instance_of: Lake
countries: United States
coordinates: lat: 37.68
lon: -119.282
surface_form: blue lake
instance_of: Lake
countries: United States
coordinates: lat: 47.017222222222
lon: -95.005
In his second expedition starting in 1843, Frémont and his party entered Oregon following the Oregon Trail. Traveling west on the Columbia River, Frémont sighted the Cascade Range peaks and mapped Mount St. Helens and Mount Hood. In early March 1844, Frèmont and his party descended the American River Valley to Sutter's Fort in Mexican California.

Geographic entities mentioned:
surface_form: Mount St. Helens
instance_of: Mountain
countries: United States
coordinates: lat: 46.200277777778
lon: -122.18944444444
surface_form: Mount Hood
instance_of: Mountain
countries: United States
coordinates: lat: 45.37361111111111
lon: -121.69583333333334
Qazi Zafar Hussain. Khan Sahib, Qazi Zafar Hussain came from a qadi's family which had, since the 16th century, been prominent among the landed aristocracy of the Soon Valley. He belonged to Awans tribe of ancient repute. He was awarded the title of Khan Sahib by the British Crown.

Geographic entities mentioned:
surface_form: Soon Valley
instance_of: Valley
countries: Pakistan
coordinates: lat: 32.58
lon: 72.15
He used his family and political influence to help the people of his area. Early life and career. He was born of famous qadi's family of Naushera, Soon Valley. He was the youngest son of Qazi Mian Muhammad Amjad, and youngest brother of 'Raees-Azam Naushera' Qazi Mazhar Qayyum. He was a descendant of Ali Ibn Abi Talib, the fourth caliph of Islam from Al-Abbas ibn Ali.

Geographic entities mentioned:
surface_form: Soon Valley
instance_of: Valley
countries: Pakistan
coordinates: lat: 32.58
lon: 72.15
The Muslim League is purely a religious movement in which all the rich, poor, Sufis and scholars are participating. Not as a pir but even as a Muslim, I have repeatedly advised Nawab Allah Baksh who is my Murid not to desert the Muslims at this critical time.&quot;
He died in 1968 at Hazel Pur, Renala Khurd, and was buried in Naushera, Soon Valley.

Geographic entities mentioned:
surface_form: Soon Valley
instance_of: Valley
countries: Pakistan
coordinates: lat: 32.58
lon: 72.15
Mount Zeppelin. kk70vb3v91owryifgdc83x5sxlvo" xml:space="preserve">#redirect Mount Zeppelin

Geographic entities mentioned:
surface_form: zeppelin
instance_of: Mountain
coordinates: lat: -64.45
lon: -61.516666666667
surface_form: mount zeppelin
instance_of: Mountain
coordinates: lat: -64.45
lon: -61.516666666667
A significant sub peak of Mount Verstovia lies just 0.5 miles to the west of the main summit. This 2,550 foot &quot;hump&quot; was reported in 1869 by G Davidson, USC&GS, to be named Cross Mountain. It is said to have acquired that name as the Russians erected a cross there. After that cross was erected, the Tlingit gave it their own name of Kanéisti Shaa (Cross Mountain).

Geographic entities mentioned:
surface_form: cross mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.576389
lon: -74.284722
surface_form: cross mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.198055555556
lon: -84.230833333333
surface_form: cross mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.832222222222
lon: -107.96861111111
surface_form: cross mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.7283
lon: -77.9918
surface_form: cross mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.080833333333
lon: -74.695833333333
surface_form: cross mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.019444444444
lon: -74.316666666667
This 2,550 foot &quot;hump&quot; was reported in 1869 by G Davidson, USC&GS, to be named Cross Mountain. It is said to have acquired that name as the Russians erected a cross there. After that cross was erected, the Tlingit gave it their own name of Kanéisti Shaa (Cross Mountain). This sub peak is now locally referred to as &quot;Picnic Rock&quot;, although it bears no name on USGS maps.

Geographic entities mentioned:
surface_form: cross mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.576389
lon: -74.284722
surface_form: cross mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.198055555556
lon: -84.230833333333
surface_form: cross mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.832222222222
lon: -107.96861111111
surface_form: cross mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.7283
lon: -77.9918
surface_form: cross mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.080833333333
lon: -74.695833333333
surface_form: cross mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.019444444444
lon: -74.316666666667
After that cross was erected, the Tlingit gave it their own name of Kanéisti Shaa (Cross Mountain). This sub peak is now locally referred to as &quot;Picnic Rock&quot;, although it bears no name on USGS maps. In hopes of avoiding confusion, modern USGS maps now name an entirely different peak approximately eight miles to the southeast as &quot;Cross Mountain&quot;. Access and recreation.

Geographic entities mentioned:
surface_form: cross mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.576389
lon: -74.284722
surface_form: cross mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.198055555556
lon: -84.230833333333
surface_form: cross mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.832222222222
lon: -107.96861111111
surface_form: cross mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.7283
lon: -77.9918
surface_form: cross mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.080833333333
lon: -74.695833333333
surface_form: cross mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.019444444444
lon: -74.316666666667
This peak was first named &quot;Gora Verstovaya&quot; in 1809 by the navigator Ivan Vasiliev. &quot;Gora&quot; translates to &quot;mount&quot; in Russian and &quot;verst&quot; refers to a unit of measurement equaling 0.6629 miles (or 3,500 feet), which closely resembles the actual height of Mt. Verstovia.

Geographic entities mentioned:
surface_form: mt. verstovia
instance_of: Mountain
countries: United States
coordinates: lat: 57.0589
lon: -135.265
Mount Verstovia. Mount Verstovia is a prominent peak located just 2.6 miles east of the center of Sitka, Alaska, on Baranof Island, Alexander Archipelago.

Geographic entities mentioned:
surface_form: mount verstovia
instance_of: Mountain
countries: United States
coordinates: lat: 57.0589
lon: -135.265
Verstovia. The main summit of Mount Verstovia is called Arrow Head by the people of Sitka, Alaska, because of its resemblance of an arrow head pointed up behind the sub peak. A significant sub peak of Mount Verstovia lies just 0.5 miles to the west of the main summit. This 2,550 foot &quot;hump&quot; was reported in 1869 by G Davidson, USC&GS, to be named Cross Mountain.

Geographic entities mentioned:
surface_form: mount verstovia
instance_of: Mountain
countries: United States
coordinates: lat: 57.0589
lon: -135.265
Access and recreation. Mount Verstovia is accessible by a well-maintained public trail that, departs from Jamestown Bay and after 1.8 miles of switchbacks, arrives at the top of &quot;Picnic Rock&quot; (USGS 2,550'). One may continue on to Mount Verstovia's summit by following the unmaintained trail approximately 0.8 miles to the east.

Geographic entities mentioned:
surface_form: mount verstovia
instance_of: Mountain
countries: United States
coordinates: lat: 57.0589
lon: -135.265
This unmaintained trail includes some steep scrambles and requires basic alpine skills and judgement. Snowboarding, skiing, and other winter sports are very popular in the bowl nestled between &quot;Picnic Rock&quot; and Mount Verstovia. The trail is marked with reflective signs on tree trunks to help snow aficionados find their way up in snowy conditions.

Geographic entities mentioned:
surface_form: mount verstovia
instance_of: Mountain
countries: United States
coordinates: lat: 57.0589
lon: -135.265
It used to have an area of and the park ended south of the Obabika River and Lower Goose Falls. It was extended south in 2005 and now has an area of. The river itself is long and continues until it empties at the north shore of and into Lake Nipissing. The town of Sturgeon Falls is located on the river about north of its mouth. The park is one of the several provincial parks in the Temagami area.

Geographic entities mentioned:
surface_form: Lake Nipissing
instance_of: Lake
countries: Canada
coordinates: lat: 46.283333333333
lon: -80
Villa Gobernador Gálvez. Villa Gobernador Gálvez is a city in the province of Santa Fe, Argentina, located on the western ravine of the Paraná River, within the metropolitan area of Greater Rosario. It had 74,509 inhabitants per the. It is separated from Rosario, to the north, by the Saladillo Stream. It is the fourth most populated city in the province and the second in the metropolitan area.

Geographic entities mentioned:
surface_form: Saladillo Stream
instance_of: Watercourse
countries: Argentina
coordinates: lat: -32.998333333333
lon: -60.611666666667
These both were established in the 1890s and played an important role in the town life. Heinolan maalaiskunta was merged into Heinola in 1997. Geography. Heinola is largely situated between two lakes, Ruotsalainen and Konnivesi. A waterway connecting the lakes crosses the town and is, along with an esker also crossing the town, a characterising geographical feature of Heinola.

Geographic entities mentioned:
surface_form: Konnivesi
instance_of: Lake
countries: Finland
coordinates: lat: 61.166667
lon: 26.15
King Vly Mountain. King Vly Mountain is a summit located in the Adirondack Mountains of New York located in the Town of Benson north-northeast of the hamlet of Upper Benson.

Geographic entities mentioned:
surface_form: vly mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.2458
lon: -74.4483
surface_form: vly mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.33646
lon: -74.36375
surface_form: king vly mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.3209
lon: -74.30375
His final international appearances would be in a 1–4 loss against Argentinos Juniors in a friendly in 1984 in preparation for the 1986 FIFA World Cup qualifiers. Later life. Bravo would later briefly manage the Peruanito Foundation within the Whittier Narrows Recreation Area of Los Angeles with several players that had played for Sporting Cristal. He died on 22 March 2019 from illness.

Geographic entities mentioned:
surface_form: Whittier Narrows Recreation Area
instance_of: Landform
countries: United States
coordinates: lat: 34.0292
lon: -118.049
census. Olivet is located immediately east of Savannah and is served by Tennessee State Route 203 and Tennessee State Route 226. The population of the CDP was 1,401 as of the 2020 census. The community was named after the Mount of Olives. Demographics. As of the 2020 census, there were 1,441 people, 624 housing units, and 513 families in the CDP.

Geographic entities mentioned:
surface_form: Mount of Olives
instance_of: Mountain
countries: Israel
coordinates: lat: 31.777946
lon: 35.245686
Populations are now located primarily in the southern portions of the United States extending into Mexico. They are considered euryhaline because they can adapt to varying salinities, ranging from freshwater lakes and swamps to brackish marshes, estuaries, and bays along the Gulf of Mexico.

Geographic entities mentioned:
surface_form: freshwater lake
instance_of: Lake
countries: Canada
coordinates: lat: 46.6453
lon: -60.3967
The fish has been sighted in eight provinces, and authorities have worked to remove it. In November 2008, a broadhead gar, genus &quot;Atractosteus&quot;, measuring was caught in the Caspian Sea north of Esenguly, Turkmenistan, by two officials of Turkmenistan Fishery Protection. On September 4, 2009, a alligator gar was found in Tak Wah Park in Tsuen Wan, Hong Kong.

Geographic entities mentioned:
surface_form: Caspian Sea
instance_of: Body of water
Lake
countries: Iran
Russia
Kazakhstan
Azerbaijan
Turkmenistan
Russian Empire
Soviet Union
coordinates: lat: 42
lon: 50.5
A necropsy will be applied to find out more. Similarly, on May 12, 2023, an alligator gar measuring less than 2 feet was caught during a deweeding process in Dal Lake of Kashmir near the Sher-i-Kashmir International Conference Centre (SKICC), sparking concerns about potential effects on the ecosystem. In Thailand, an alligator gar have long been considered an imported aquarium fish.

Geographic entities mentioned:
surface_form: Dal Lake
instance_of: Lake
countries: India
coordinates: lat: 34.12
lon: 74.87
Population: 14,951 (2002 Census);
Geography. The district is elongated from west to east and lies in the basin of the Sukhona River. The westernmost part of the district is on the shore of Lake Kubenskoye. The source of the Sukhona is located in Ust-Kubinsky District, but a relatively short stretch of the river course runs through the district downstream of the source.

Geographic entities mentioned:
surface_form: Lake Kubenskoye
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 59.640277777778
lon: 39.446944444444
Lake Maratanza. Lake Maratanza is the highest lake in New York's Shawangunk Ridge at above sea level. It is within Sam's Point Preserve. The lake is dammed and supplies drinking water to Ellenville. The outlet brook drains to the other side of the ridge, into the Verkeerder Kill, a tributary of the Shawangunk Kill and by extension the Wallkill River.

Geographic entities mentioned:
surface_form: lake maratanza
instance_of: Lake
countries: United States
coordinates: lat: 41.680155555556
lon: -74.352808333333
Much of the lake's watershed is owned and managed by the Michigan Department of Natural Resources (M-DNR). The lake is technically a reservoir; a dam at the Wycamp Creek outlet controls the flowage of the lake's water to Lake Michigan.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
surface_form: michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Wycamp Lake. Wycamp Lake is a shallow lake in Emmet County in the U.S. state of Michigan. in size, it is located approximately northeast of Cross Village, Michigan. It is located within Mackinaw State Forest and is served by local unimproved roads and by the North Country Trail. A typical shallow lake in the North Woods, the lake is partly surrounded by wetlands.

Geographic entities mentioned:
surface_form: shallow lake
instance_of: Lake
countries: United States
coordinates: lat: 43.49
lon: -74.444
surface_form: michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
surface_form: wycamp lake
instance_of: Lake
countries: United States
coordinates: lat: 45.66084
lon: -84.9655
It is located within Mackinaw State Forest and is served by local unimproved roads and by the North Country Trail. A typical shallow lake in the North Woods, the lake is partly surrounded by wetlands. Like much of the Mackinaw State Forest, the region around the lake was cut over in the late 1800s for timber; exhausted land parcels were allowed to return to the public sector.

Geographic entities mentioned:
surface_form: shallow lake
instance_of: Lake
countries: United States
coordinates: lat: 43.49
lon: -74.444
Wycamp Lake. Wycamp Lake is a shallow lake in Emmet County in the U.S. state of Michigan. in size, it is located approximately northeast of Cross Village, Michigan. It is located within Mackinaw State Forest and is served by local unimproved roads and by the North Country Trail. A typical shallow lake in the North Woods, the lake is partly surrounded by wetlands.

Geographic entities mentioned:
surface_form: michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
A typical shallow lake in the North Woods, the lake is partly surrounded by wetlands. Like much of the Mackinaw State Forest, the region around the lake was cut over in the late 1800s for timber; exhausted land parcels were allowed to return to the public sector. Much of the lake's watershed is owned and managed by the Michigan Department of Natural Resources (M-DNR).

Geographic entities mentioned:
surface_form: michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
The lake is technically a reservoir; a dam at the Wycamp Creek outlet controls the flowage of the lake's water to Lake Michigan. The creek and lake shoreline have been inhabited for centuries, and the Wycamp Creek Site, a Lake Michigan shoreline campsite by the lake's creek outlet, has been listed on the National Register of Historic Places.

Geographic entities mentioned:
surface_form: michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
surface_form: lake michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Wycamp Lake. Wycamp Lake is a shallow lake in Emmet County in the U.S. state of Michigan. in size, it is located approximately northeast of Cross Village, Michigan. It is located within Mackinaw State Forest and is served by local unimproved roads and by the North Country Trail. A typical shallow lake in the North Woods, the lake is partly surrounded by wetlands.

Geographic entities mentioned:
surface_form: wycamp lake
instance_of: Lake
countries: United States
coordinates: lat: 45.66084
lon: -84.9655
The creek and lake shoreline have been inhabited for centuries, and the Wycamp Creek Site, a Lake Michigan shoreline campsite by the lake's creek outlet, has been listed on the National Register of Historic Places. Stone tools excavated at the site could have been used to hunt birds, and Wycamp Lake is a noted bird-hunting location to this day.

Geographic entities mentioned:
surface_form: wycamp lake
instance_of: Lake
countries: United States
coordinates: lat: 45.66084
lon: -84.9655
Mountelgonia percivali. &quot;Mountelgonia percivali&quot; is a moth of the family Cossidae. It is found from the areas east of the summits of Mount Elgon to the western highlands of Kenya. It is probably also found on the western side of Mount Elgon in Uganda. The habitat consists of dry Afromontane forest at high altitudes. The wingspan is about 22 mm for males and 26.5 mm for females.

Geographic entities mentioned:
surface_form: Mount Elgon
instance_of: Mountain
countries: Uganda
Kenya
coordinates: lat: 1.1185
lon: 34.5265
Rugg Peak. Rugg Peak () is a peak on the east side of Widmark Ice Piedmont south of Crookes Peak, on the west coast of Graham Land. Photographed by Hunting Aerosurveys Ltd in 1956–57, it was mapped from these photos by the Falkland Islands Dependencies Survey (FIDS).

Geographic entities mentioned:
surface_form: Crookes Peak
instance_of: Mountain
coordinates: lat: -66.2333
lon: -65.3
surface_form: rugg peak
instance_of: Mountain
coordinates: lat: -66.3167
lon: -65.3833
Rugg Peak. Rugg Peak () is a peak on the east side of Widmark Ice Piedmont south of Crookes Peak, on the west coast of Graham Land. Photographed by Hunting Aerosurveys Ltd in 1956–57, it was mapped from these photos by the Falkland Islands Dependencies Survey (FIDS).

Geographic entities mentioned:
surface_form: rugg peak
instance_of: Mountain
coordinates: lat: -66.3167
lon: -65.3833
Logan Glacier (Alaska). Logan Glacier is a glacier in the U.S. state of Alaska and territory of Yukon, Canada. It heads down the northern side of the Mount Logan massif in the Yukon, flowing northwest across the Canada-United States boundary to form the headwaters of the Chitina River. It was named for its origin on the slopes of, and proximity to, Mount Logan.

Geographic entities mentioned:
surface_form: Mount Logan
instance_of: Mountain
countries: Canada
coordinates: lat: 60.567222222222
lon: -140.40277777778