Sarmila/GeoWiki-Features huggingface dataset:
In the first millennium BC, Phoenicians and Greeks established colonies throughout the Mediterranean and the Black Sea. Around 500 BC, the Carthaginian navigator Hanno left a detailed periplus of an Atlantic journey that reached at least Senegal and possibly Mount Cameroon.

Geographic entities mentioned:
surface_form: Mount Cameroon
instance_of: Mountain
countries: Cameroon
coordinates: lat: 4.2166666666667
lon: 9.1725
Large quantities of goods are transported by sea, especially across the Atlantic and around the Pacific Rim. A major trade route passes through the Pillars of Hercules, across the Mediterranean and the Suez Canal to the Indian Ocean and through the Straits of Malacca; much trade also passes through the English Channel.

Geographic entities mentioned:
surface_form: Pillars of Hercules
instance_of: Landform
countries: Morocco
Spain
Gibraltar
coordinates: lat: 36
lon: -5.35
Shoreline features include beach ridges, river deltas, spits and wavecut platforms. After the shrinkage of Lake Palomas and its successor lakes, wind erosion has occurred on the shoreline deposits. The eroded particles formed the Samalayuca Dune Fields upon deposition. Climate. The present-day climate of the Lake Palomas area is cold in winter and hot in summer.

Geographic entities mentioned:
surface_form: Samalayuca Dune Fields
instance_of: Mountain
countries: Mexico
coordinates: lat: 31.14
lon: -106.9
History. Before Lake Palomas, an even larger lake existed in the area, Lake Cabeza de Vaca. Named after Álvar Núñez Cabeza de Vaca, this lake covered a surface area of in Chihuahua and New Mexico. It was nourished by the Rio Grande through the Mesilla Valley and its shores approximately followed the present-day contours. Lake Palomas itself is considered to have formed 500,000 years ago.

Geographic entities mentioned:
surface_form: Mesilla Valley
instance_of: Valley
countries: United States
coordinates: lat: 31.7903
lon: -106.423
Lake Palomas. Lake Palomas is a former lake in New Mexico, United States, and Chihuahua, Mexico. This lake was relatively large and reached a size of about during its highstands. Preceded by Lake Cabeza de Vaca, it formed during the Pleistocene and continued into the Holocene, when several different lake phases occurred. Presently its basin is a major source of airborne dust in the region. Name.

Geographic entities mentioned:
surface_form: lake palomas
instance_of: Body of water
countries: Mexico
United States
coordinates: lat: 31.22
lon: -106.99
Preceded by Lake Cabeza de Vaca, it formed during the Pleistocene and continued into the Holocene, when several different lake phases occurred. Presently its basin is a major source of airborne dust in the region. Name. Lake Palomas is named after Puerto Palomas, Chihuahua. The northwestern part of the Lake Palomas basin is also known as &quot;Guzmán Sink&quot;. Hydrogeography.

Geographic entities mentioned:
surface_form: lake palomas
instance_of: Body of water
countries: Mexico
United States
coordinates: lat: 31.22
lon: -106.99
Presently its basin is a major source of airborne dust in the region. Name. Lake Palomas is named after Puerto Palomas, Chihuahua. The northwestern part of the Lake Palomas basin is also known as &quot;Guzmán Sink&quot;. Hydrogeography. During highstands the lake was about long and in some places wide. It covered a surface area possibly over during these highstands and at lowstands.

Geographic entities mentioned:
surface_form: lake palomas
instance_of: Body of water
countries: Mexico
United States
coordinates: lat: 31.22
lon: -106.99
At these sizes it was one of the largest pluvial lakes in the southwestern United States during the late Pleistocene. Most of the lake was located in Mexico, with only a bay between the West Potrillo Mountains and the Tres Hermanas Mountains extending into New Mexico. At highstand, Lake Palomas contained the islands Unión and Santa María. The islands were and, respectively.

Geographic entities mentioned:
surface_form: lake palomas
instance_of: Body of water
countries: Mexico
United States
coordinates: lat: 31.22
lon: -106.99
The lake was subdivided into three basins (east, central and west) by upthrust Cretaceous mountains and Tertiary intrusives. None of these basins were very deep during the history of Lake Palomas; the deepest point during La Mota time was in Salinas de Unión where the current basin floor is beneath the La Mota shoreline.

Geographic entities mentioned:
surface_form: lake palomas
instance_of: Body of water
countries: Mexico
United States
coordinates: lat: 31.22
lon: -106.99
surface_form: lake palomas
instance_of: Body of water
countries: Mexico
United States
coordinates: lat: 31.22
lon: -106.99
Inflow. The Río Casas Grandes, Río del Carmen, Mimbres River or Río Santa María either drained into Lake Palomas or had part of their course submerged by it. The catchment of Lake Palomas covered about, and was fully developed by about 200,000 years ago. Shorelines. Three different shorelines of Lake Palomas are known. These are the La Mota, the Guzmán and the Las Muertos at.

Geographic entities mentioned:
surface_form: lake palomas
instance_of: Body of water
countries: Mexico
United States
coordinates: lat: 31.22
lon: -106.99
The catchment of Lake Palomas covered about, and was fully developed by about 200,000 years ago. Shorelines. Three different shorelines of Lake Palomas are known. These are the La Mota, the Guzmán and the Las Muertos at. The La Mota shorelines are noticeable on the northeastern side of the lake between Columbus, New Mexico, and Villa Ahumada, Chihuahua, where they are over.

Geographic entities mentioned:
surface_form: lake palomas
instance_of: Body of water
countries: Mexico
United States
coordinates: lat: 31.22
lon: -106.99
Shoreline features include beach ridges, river deltas, spits and wavecut platforms. After the shrinkage of Lake Palomas and its successor lakes, wind erosion has occurred on the shoreline deposits. The eroded particles formed the Samalayuca Dune Fields upon deposition. Climate. The present-day climate of the Lake Palomas area is cold in winter and hot in summer.

Geographic entities mentioned:
surface_form: lake palomas
instance_of: Body of water
countries: Mexico
United States
coordinates: lat: 31.22
lon: -106.99
The eroded particles formed the Samalayuca Dune Fields upon deposition. Climate. The present-day climate of the Lake Palomas area is cold in winter and hot in summer. Precipitation totals about, with high elevation areas reaching twice to thrice as much as lowland. Precipitation falls mostly in summer; the winter precipitation is controlled by the El Nino-Southern Oscillation.

Geographic entities mentioned:
surface_form: lake palomas
instance_of: Body of water
countries: Mexico
United States
coordinates: lat: 31.22
lon: -106.99
Precipitation totals about, with high elevation areas reaching twice to thrice as much as lowland. Precipitation falls mostly in summer; the winter precipitation is controlled by the El Nino-Southern Oscillation. Lake levels at Lake Palomas were controlled by the position of the polar jet stream, which could drive storm systems into the region when it was positioned farther south.

Geographic entities mentioned:
surface_form: lake palomas
instance_of: Body of water
countries: Mexico
United States
coordinates: lat: 31.22
lon: -106.99
The increased cloud cover and lower temperatures reduced evaporation and the storms added precipitation to the basin, causing lake levels to increase. The North American Monsoon on the other hand does not appear to have played a major role in the lake history, seeing as lake levels of Lake Palomas are correlated to lake levels in basins such as Silver Lake that are not monsoonally influenced.

Geographic entities mentioned:
surface_form: lake palomas
instance_of: Body of water
countries: Mexico
United States
coordinates: lat: 31.22
lon: -106.99
The large size of Lake Palomas and its subsequent fragmentation had strong effects on the development of animal species inhabiting its basin, forming isolated clades. &quot;Cyprinodon pisteri&quot;, beautiful shiner, largemouth shiner and red shiner exist within the catchment of Lake Palomas and may have developed from a common ancestor that lived in the lake and its catchment.

Geographic entities mentioned:
surface_form: lake palomas
instance_of: Body of water
countries: Mexico
United States
coordinates: lat: 31.22
lon: -106.99
surface_form: lake palomas
instance_of: Body of water
countries: Mexico
United States
coordinates: lat: 31.22
lon: -106.99
&quot;Cyprinodon pisteri&quot;, beautiful shiner, largemouth shiner and red shiner exist within the catchment of Lake Palomas and may have developed from a common ancestor that lived in the lake and its catchment. The fragmentation of Lake Palomas would have triggered the split into various species. History. Before Lake Palomas, an even larger lake existed in the area, Lake Cabeza de Vaca.

Geographic entities mentioned:
surface_form: lake palomas
instance_of: Body of water
countries: Mexico
United States
coordinates: lat: 31.22
lon: -106.99
It was nourished by the Rio Grande through the Mesilla Valley and its shores approximately followed the present-day contours. Lake Palomas itself is considered to have formed 500,000 years ago. The La Mota shoreline of Lake Palomas is approximately coeval with Lake Lahontan and Lake Bonneville, about 60,000 years before present.

Geographic entities mentioned:
surface_form: lake palomas
instance_of: Body of water
countries: Mexico
United States
coordinates: lat: 31.22
lon: -106.99
Lake Palomas reformed during the early Holocene, covering a surface area of at that point. Other lakes in the region also show a highstand at that time, which at Lake Palomas is dated to 9,255 to 9,430 years ago. Additional lake stands are recorded during the mid-Holocene, the Neoglacial and the Little Ice Age.

Geographic entities mentioned:
surface_form: lake palomas
instance_of: Body of water
countries: Mexico
United States
coordinates: lat: 31.22
lon: -106.99
The mid-Holocene stand is unusual as other evidence indicates a dry time period. Present day. The Bolsón de Los Muertos is the largest present-day basin in the area of Lake Palomas. Other basins such as Guzmán playa, Indian Basin, Patos Playa, Sabinal Playa (also known as Laguna El Fresnal) and Santa María Playa presently cover the floor of Lake Palomas.

Geographic entities mentioned:
surface_form: lake palomas
instance_of: Body of water
countries: Mexico
United States
coordinates: lat: 31.22
lon: -106.99
Present day. The Bolsón de Los Muertos is the largest present-day basin in the area of Lake Palomas. Other basins such as Guzmán playa, Indian Basin, Patos Playa, Sabinal Playa (also known as Laguna El Fresnal) and Santa María Playa presently cover the floor of Lake Palomas. During El Niño events these basins can flood, forming ephemeral lakes that last for weeks.

Geographic entities mentioned:
surface_form: lake palomas
instance_of: Body of water
countries: Mexico
United States
coordinates: lat: 31.22
lon: -106.99
Caudal Hills. x0kn2frdklp1582v1kwr8p50c3mx" xml:space="preserve">The Caudal Hills () are a group of hills situated within Victoria Land, Antarctica the hills lie between the Sequence Hills and the Lichen Hills on the western margin of upper Rennick Glacier. A series of spurs &quot;tail&quot; out to the north, hence the name &quot;Caudal&quot;.

Geographic entities mentioned:
surface_form: Sequence Hills
instance_of: Mountain
coordinates: lat: -73.05
lon: 161.25
Higgins Pond. Higgins Pond is a kettle pond in Brewster, Massachusetts. It is located in Nickerson State Park. The Massachusetts Division of Fisheries and Wildlife stocks the pond in spring with various trout species. Access to the pond is difficult for vehicles, but the pond offers anglers good wading.

Geographic entities mentioned:
surface_form: higgins pond
instance_of: Lake
countries: United States
coordinates: lat: 41.758055555556
lon: -70.009444444444
Triveni Sangam in Tamil Nadu. The Triveni Sangam in Kooduthurai, Erode, Tamil Nadu is a confluence of the Kaveri, Bhavani and Amudha and is known as the South Indian Triveni Sangam, or &quot;Dakshina Sangam&quot;. Nepal. Triveni Dham is a confluence of three rivers, Sona, Tamasa and Sapta Gandaki located in Binayi Tribeni Rural Municipality, Nawalparasi district of Nepal. Bhagamandala.

Geographic entities mentioned:
surface_form: Kaveri
instance_of: Watercourse
countries: India
coordinates: lat: 11.370345
lon: 79.828105
Bhagamandala. Bhagamandala is a pilgrimage place in Kodagu district of Karnataka. It is situated on the river Kaveri in its upstream stretches. At this place, the Kaveri is joined by two tributaries, the Kannike and the Sujyoti river. It is considered sacred as a river confluence (&quot;kudala&quot; or &quot;triveni sangama&quot;, in Kannada and Sanskrit respectively). Tirumakudalu Narasipura.

Geographic entities mentioned:
surface_form: Kaveri
instance_of: Watercourse
countries: India
coordinates: lat: 11.370345
lon: 79.828105
Narasipura, is a panchayat town in Mysore district in the Indian state of Karnataka. The first name refers to the land at the confluence (&quot;trimakuta&quot; in Sanskrit) at the confluence of the Kaveri, Kabini and Spatika Sarovara (a lake or spring, also named Gupta Gamini). This is the place in South India where local Kumbhamela is held every three years. Moovattupuzha.

Geographic entities mentioned:
surface_form: Kaveri
instance_of: Watercourse
countries: India
coordinates: lat: 11.370345
lon: 79.828105
It may be found both in fresh and brackish waters between the Kolyma River and the Bering Sea, including the Rauchua (Bilibino District), the Chaun Bay rivers (Chaun District), Pegtymel River, Amguema River, Vankarem River and Kymyneyveem River (Iultinsky District), as well as the rivers of the Kolyuchin Bay, Chegitun River, Uttyveem River and Koolenvaam River, the Saint Lawrence Bay, Mechigmen Bay, Getlyangen, Lake Achchyon, Nunyamovaam and Erguveem (Providensky District) and Seutakan, Chelkun and Ioniveyem River.

Geographic entities mentioned:
surface_form: Achchyon
instance_of: Body of water
countries: Russia
coordinates: lat: 64.8075
lon: -174.68277777778
Vegan Treats Bakery has been in operation since 1998. The bakery is completely vegan, using no animal by-products in any of its goods. Vegan Treats owner Danielle Konya grew up in Northampton County, Pennsylvania, and has kept her business local in the Lehigh Valley. Konya's desserts have earned her a PETA Proggy Award for Best Bakery.

Geographic entities mentioned:
surface_form: Lehigh Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.7
lon: -75.5
Kleiner Feldberg. The Kleiner Feldberg is the second-highest mountain in the Taunus mountain range, located in Hesse, Germany. It has an elevation of. The Großer Feldberg is located in its immediate neighbourhood. Obeservatory. In 1913, a meteorological and geophysical observatory was built there by German meteorologist Franz Linke.

Geographic entities mentioned:
surface_form: Großer Feldberg
instance_of: Mountain
countries: Germany
coordinates: lat: 50.2325
lon: 8.4588888888889
surface_form: feldberg
instance_of: Mountain
countries: Germany
coordinates: lat: 51.0739
lon: 7.91028
surface_form: feldberg
instance_of: Mountain
countries: Germany
coordinates: lat: 50.356
lon: 10.022
surface_form: feldberg
instance_of: Mountain
countries: Germany
coordinates: lat: 47.873611111111
lon: 8.0038888888889
surface_form: feldberg
instance_of: Mountain
countries: Germany
coordinates: lat: 50.4719
lon: 9.9509
Kleiner Feldberg. The Kleiner Feldberg is the second-highest mountain in the Taunus mountain range, located in Hesse, Germany. It has an elevation of. The Großer Feldberg is located in its immediate neighbourhood. Obeservatory. In 1913, a meteorological and geophysical observatory was built there by German meteorologist Franz Linke.

Geographic entities mentioned:
surface_form: feldberg
instance_of: Mountain
countries: Germany
coordinates: lat: 51.0739
lon: 7.91028
surface_form: feldberg
instance_of: Mountain
countries: Germany
coordinates: lat: 50.356
lon: 10.022
surface_form: kleiner feldberg
instance_of: Mountain
countries: Germany
coordinates: lat: 50.221666666667
lon: 8.4458333333333
surface_form: feldberg
instance_of: Mountain
countries: Germany
coordinates: lat: 47.873611111111
lon: 8.0038888888889
surface_form: feldberg
instance_of: Mountain
countries: Germany
coordinates: lat: 50.4719
lon: 9.9509
Lessons learned on Iwo Jima served as guidelines for American forces in the Battle of Okinawa two months later and the planned invasion of the Japanese homeland. Joe Rosenthal's Associated Press photograph of the raising of the U.S. flag at the summit of the Mount Suribachi by six Marines became a famous image of the battle and the American war in the Pacific. Background.

Geographic entities mentioned:
surface_form: Mount Suribachi
instance_of: Mountain
countries: Japan
coordinates: lat: 24.749030555556
lon: 141.28778333333
Takeichi Nishi's armored tanks were camouflaged and used as static artillery positions. Because the tunnel linking Mount Suribachi to the rest of the island was never completed, Kuribayashi organized the southern area of the island in and around the mountain as a semi-independent sector, with his main defensive zone built up in the north.

Geographic entities mentioned:
surface_form: Mount Suribachi
instance_of: Mountain
countries: Japan
coordinates: lat: 24.749030555556
lon: 141.28778333333
The park lies entirely in the drainage basin of the Po River. It is located between the valley of Vigezzo in the north, the Cannobina valley in the northwest, the valley of Ossola in the southwest, and Lake Maggiore in the southeast. The park is not populated and is often described as &quot;the largest wilderness in the Alps&quot;.

Geographic entities mentioned:
surface_form: Vigezzo
instance_of: Valley
countries: Italy
coordinates: lat: 46.1333
lon: 8.55
surface_form: Ossola
instance_of: Valley
countries: Italy
coordinates: lat: 46.283333333333
lon: 8.35
surface_form: Lake Maggiore
instance_of: Lake
countries: Switzerland
Italy
coordinates: lat: 46.098055555555554
lon: 8.714722222222223
Lake Amador. Lake Amador is a reservoir located in Amador County, California. It lies at an elevation of 325 feet. The lake's water is impounded by the Jackson Creek Dam, a tall earth-and-rock dam, built in 1965 across Jackson Creek. The dam is long and wide and contains of material. Its crest is about sea level, and it belongs to the Jackson Valley Irrigation District.

Geographic entities mentioned:
surface_form: lake amador
instance_of: Lake
countries: United States
coordinates: lat: 38.3033
lon: -120.889
The dam is long and wide and contains of material. Its crest is about sea level, and it belongs to the Jackson Valley Irrigation District. The reservoir's capacity is. Lake Amador was the site of the Gold Rush rock music festival on October 4, 1969. Performers included Ike & Tina Turner, Santana, Bo Diddley, Albert Collins, and Taj Mahal.

Geographic entities mentioned:
surface_form: lake amador
instance_of: Lake
countries: United States
coordinates: lat: 38.3033
lon: -120.889
Commercial stocking has introduced it to other areas of Italy, often alongside &quot;E. lucius&quot;. Historically recovered specimens from southeastern France and Lake Geneva have also been assigned to this species. &quot;E. cisalpinus&quot; has also been introduced to areas outside of its native range.

Geographic entities mentioned:
surface_form: Lake Geneva
instance_of: Lake
countries: Switzerland
France
coordinates: lat: 46.45
lon: 6.55
It was built in 1828 and is a two-story, five bay Federal style brick structure featuring a recessed entrance. Built originally as a tavern on the stagecoach lines of the Finger Lakes Region, it was later modified for use as Bethesda Sanitarium and operated by Dr. Charles Deland Clawson. In 1974, it became home to the Schuyler County Historical Society.

Geographic entities mentioned:
surface_form: Finger Lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 42.666666666667
lon: -76.833333333333
History. The Tanana Valley Fair was founded in 1924, making it the oldest state fair in Alaska. Experimental agronomist George William Gasser and local real estate businessman and homesteading farmer Harry Markley Badger were instrumental in forming the not-for-profit Tanana Valley Fair Association. From 1924 to 1951, the fair was held in various locations in downtown Fairbanks.

Geographic entities mentioned:
surface_form: Tanana Valley
instance_of: Valley
countries: United States
coordinates: lat: 64.4
lon: -147
In 1990, CKOA became CHVR-2, as CKOB Renfrew became CHVR-1 and both stations were then re-broadcasters of CHVR in Pembroke. In 1996, CHVR and the former CKOA and CKOB were combined into a new FM radio station at 96.7 MHz as CHVR-FM out of Pembroke to serve the Ottawa Valley. All three AM transmitters were deleted after the new FM station signed on.

Geographic entities mentioned:
surface_form: Ottawa Valley
instance_of: Valley
countries: Canada
coordinates: lat: 45.91682
lon: -77.13276
It is situated in the Oruro Department, Sajama Province, Turco Municipality, north-east of Umurata and south of the Bolivian Route 4 that leads to Tambo Quemado on the border with Chile.

Geographic entities mentioned:
surface_form: Umurata
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -18.355555555556
lon: -69.049722222222
Kuntur Ikiña (Sajama). Kuntur Ikiña (Aymara &quot;kunturi&quot; condor, &quot;ikiña&quot; to sleep, bed or blanket, &quot;bed of the condor&quot; or &quot;resting place of the condor&quot;, Hispanicized spelling &quot;Condor Iquiña&quot;) is a mountain in the Andes located in the Cordillera Occidental of Bolivia.

Geographic entities mentioned:
surface_form: kuntur ikiña
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.33333333
lon: -69
surface_form: sajama
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.108055555556
lon: -68.883055555556
surface_form: kuntur ikiña
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.66805556
lon: -66.82027778
Kuntur Ikiña (Sajama). Kuntur Ikiña (Aymara &quot;kunturi&quot; condor, &quot;ikiña&quot; to sleep, bed or blanket, &quot;bed of the condor&quot; or &quot;resting place of the condor&quot;, Hispanicized spelling &quot;Condor Iquiña&quot;) is a mountain in the Andes located in the Cordillera Occidental of Bolivia.

Geographic entities mentioned:
surface_form: kuntur ikiña
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.33333333
lon: -69
surface_form: kuntur ikiña
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.66805556
lon: -66.82027778
In the first engagement, in Porto Torres, the Pisans were victorious. Pisa secured a papal privilege and strengthened their control over the island by installing monks from Saint-Victor de Marseille and expelling all those monks from rival Monte Cassino whom they could capture. Her interest in curtailing Islamic piracy did not stop at Sardinia. In 1034 her fleet destroyed the pirate base of Bône.

Geographic entities mentioned:
surface_form: Monte Cassino
instance_of: Mountain
countries: Italy
coordinates: lat: 41.49
lon: 13.813888888889
The Kurdish regiments that accompanied Salidin established self-ruled areas in and around Damascus. These settlements evolved into the Kurdish sections of Damascus of &quot;Hayy al-Akrad&quot; (the Kurdish quarter) and the Salhiyya districts located in the north-east of Damasacus on Mount Qasioun. Ottoman period. The Kurdish community's role in the military continued under the Ottomans.

Geographic entities mentioned:
surface_form: Mount Qasioun
instance_of: Mountain
countries: Syria
coordinates: lat: 33.545833333333
lon: 36.286388888889
Other major infrastructures includes the opening of the Hong Kong Disneyland in 2005, which was the fifth Disneyland opened in the world and the second opened in Asia after the Tokyo Disneyland, and the completion of the Ngong Ping 360 in 2006, which was a gondola lift system that connects Tung Chung New Town and Ngong Ping Market. Population. In 2000, the population of Hong Kong was 6,900,000.

Geographic entities mentioned:
surface_form: Ngong Ping
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 22.2554
lon: 113.904
Tulare Lake (Alameda County). Tulare Lake was a large, shallow lake in the center of the Amador Valley, surrounded by Willow Marsh (also known as the Lagoon). Tule rushes and willow trees once lined the marshes and sloughs of its shores.

Geographic entities mentioned:
surface_form: Amador Valley
instance_of: Valley
countries: United States
coordinates: lat: 37.6831
lon: -121.874
surface_form: tulare lake
instance_of: Lake
countries: United States
coordinates: lat: 37.666666666666664
lon: -121.9
The lake was fed by the runoff of the entire Amador Valley, as well as the Arroyo Mocho and the Arroyo Valle. Its outlet was the Arroyo de la Laguna, which flowed for a short distance before joining Alameda Creek. The Tulare Lake area (Amador Valley and Livermore Valley) was inhabited by groups of the Ohlone people prior to the 19th century, in particular the Pelnen tribe near Pleasanton.

Geographic entities mentioned:
surface_form: Amador Valley
instance_of: Valley
countries: United States
coordinates: lat: 37.6831
lon: -121.874
surface_form: Livermore Valley
instance_of: Valley
countries: United States
coordinates: lat: 37.6886
lon: -121.736
surface_form: tulare lake
instance_of: Lake
countries: United States
coordinates: lat: 37.666666666666664
lon: -121.9
Such rapid developments have led to large seasonal flow variations in Niles Canyon. The lake was fed by the runoff of the entire Amador Valley, as well as the Arroyo Mocho and the Arroyo Valle. Its outlet was the Arroyo de la Laguna, which flowed for a short distance before joining Alameda Creek.

Geographic entities mentioned:
surface_form: amador valley
instance_of: Valley
countries: United States
coordinates: lat: 37.6831
lon: -121.874
Tulare Lake (Alameda County). Tulare Lake was a large, shallow lake in the center of the Amador Valley, surrounded by Willow Marsh (also known as the Lagoon). Tule rushes and willow trees once lined the marshes and sloughs of its shores.

Geographic entities mentioned:
surface_form: tulare lake (alameda county)
instance_of: Lake
countries: United States
coordinates: lat: 37.666666666666664
lon: -121.9
Initially, floodwater discharged from Glacial Lake Columbia by running up through the head of Grand Coulee and down through Foster Coulee to rejoin the Columbia River. After the floods, meltwater from the glacier reversed course and flowed east through the coulee, forming a hanging valley above the west rim of Grand Coulee and a debris fan on the Grand Coulee floor that can be seen today.

Geographic entities mentioned:
surface_form: Grand Coulee
instance_of: Valley
countries: United States
coordinates: lat: 47.62
lon: -119.308
In 2009 only Knaupsholz granite was still being quarried. Geology. The granitic plutons of the Harz Mountains - the Brocken, Ramberg and Oker plutons - were formed at the end of the Harz mountain building period (the Hercynian orogeny) during the Late Carboniferous about 300 million years ago.

Geographic entities mentioned:
surface_form: Brocken
instance_of: Mountain
countries: Germany
Kingdom of Prussia
coordinates: lat: 51.800555555556
lon: 10.617222222222
In the early 1950s, the following quarries in the Brocken granite region were listed by Sickenberg (1951): &quot;Eckerloch, Schneeloch, Gebbertsberg, Wurmberg, Haserode, Wolfklippen, Großer und Kleiner Birkenkopf, Knaupsholz, Ottofels, Neustätter Hau, Forsthaus Plessenburg&quot; and &quot;Gelochter Stein&quot;.

Geographic entities mentioned:
surface_form: Eckerloch
instance_of: Valley
countries: Germany
coordinates: lat: 51.785
lon: 10.617812
Hadley Rille (also referred to as Rima Hadley) is located to the west of the Apollo 15 landing site and was the subject of substantial investigation during that mission. The feature, named from nearby Mons Hadley, is a channel that was likely formed by volcanic processes earlier in the history of the Moon. Apollo 15 landing site.

Geographic entities mentioned:
surface_form: Mons Hadley
instance_of: Mountain
coordinates: lat: 26.69
lon: 4.12
Apollo 15 landing site. The American Apollo 15 mission, the first of the J-series missions that featured both increased scientific capability and the use of the Lunar Roving Vehicle, landed in an area of the Hadley–Apennine region to the west of the Apennine Front situated between the mountains Mons Hadley and Mons Hadley Delta to the northeast and south, respectively.

Geographic entities mentioned:
surface_form: Mons Hadley Delta
instance_of: Mountain
coordinates: lat: 25.72
lon: 3.71
Kotcho Formation. The Kotcho Formation is a stratigraphic unit of middle Famennian age in the Western Canadian Sedimentary Basin. It takes the name from Kotcho Lake and was first described in the &quot;Imperial Island River No. 1&quot; by H.R. Belyea and D.J. McLaren in 1962. Lithology.

Geographic entities mentioned:
surface_form: Kotcho Lake
instance_of: Lake
countries: Canada
coordinates: lat: 59.068333333333
lon: -121.14944444444
Northeastern Pennsylvania borders the Pennsylvania Wilds to the west, the New York State Southern Tier and Hudson Valley regions to the north and northeast, Sussex and Warren counties in New Jersey to the east, and the Lehigh Valley to the south. Area.

Geographic entities mentioned:
surface_form: Hudson Valley
instance_of: Valley
countries: United States
coordinates: lat: 41.9209
lon: -73.9613
surface_form: Lehigh Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.7
lon: -75.5
Ben Tianavaig. Ben Tianavaig is a hill located on the Isle of Skye, near Portree. It is very prominent from Portree dominating the view from the harbour. It is a Marilyn (a hill with topographic prominence of at least 150m). It is most simply ascended from Camastianavaig. Despite its proximity to dwellings one could expect to see golden eagles and sea eagles from its ridge.

Geographic entities mentioned:
surface_form: ben tianavaig
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.3902
lon: -6.1437388888889
Latrigg. Latrigg is one of the lowest fells in the Lake District in North West England, but is a popular climb due to its convenient location overlooking the town of Keswick and the beautiful views down the valley of Borrowdale from the summit. It is the least mountainous of the Skiddaw fells, the summit being almost entirely devoid of rock.

Geographic entities mentioned:
surface_form: Skiddaw
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.651388888889
lon: -3.1477777777778
It takes the form of a rounded hump at the terminus of a long descending ridge, and would be unremarkable if not for its location. To the north of Latrigg summit is an unnamed depression at about and rising beyond is a grassy rigg, climbing up to Jenkin Hill and the top of Skiddaw Little Man. Latrigg itself sends out a narrow ridge to the east, about a mile long and ending at Brundholm.

Geographic entities mentioned:
surface_form: Skiddaw Little Man
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.639061111111
lon: -3.1387611111111
Latrigg itself sends out a narrow ridge to the east, about a mile long and ending at Brundholm. The fell is bordered by the two streams falling from the northern col. Gale Gill runs west to join the River Derwent between Derwentwater and Bassenthwaite Lake. The unnamed eastern stream joins Whit Beck and then flows into the River Greta, bound again for the Derwent via Keswick.

Geographic entities mentioned:
surface_form: Derwentwater
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.583333333333
lon: -3.15
surface_form: Bassenthwaite Lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.652
lon: -3.215
A ditch and parapet run across the top. The parapet was the base of a fence, long since decayed, and the ditch was the source of the earth for its construction. The view northward is of the high grassy flanks of Skiddaw and Blencathra, impressive but lacking detail. To the south the contrast is total.

Geographic entities mentioned:
surface_form: Blencathra
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.63985
lon: -3.0504611111111
History. USS &quot;Sangay&quot; was named after the Sangay volcano in Ecuador, a tongue-in-cheek reference to what would happen if a munitions ship was hit by enemy fire. She was laid down under Maritime Commission contract (MC hull 225) as &quot;Cape Sable&quot; on 30 October 1941 by Pennsylvania Shipyards, Inc., Beaumont, Texas; launched on 5 April 1942; sponsored by Mrs. A.

Geographic entities mentioned:
surface_form: Sangay
instance_of: Mountain
countries: Ecuador
coordinates: lat: -2.0025
lon: -78.340833333333
Bartibog River. The Bartibog River (also spelled Bartibogue) is a tributary of the Miramichi River in New Brunswick, Canada. It honours Bartholomew La Bogue, a Micmac chief, &quot;who was called Balt Bogue by the Indians (indigenous) and Bartabogue by the French and English&quot; (Rayburn)&quot;.

Geographic entities mentioned:
surface_form: bartibog river
instance_of: Watercourse
countries: Canada
coordinates: lat: 47.1086
lon: -65.3707
It honours Bartholomew La Bogue, a Micmac chief, &quot;who was called Balt Bogue by the Indians (indigenous) and Bartabogue by the French and English&quot; (Rayburn)&quot;. The Bartibog River rises in northeastern Northumberland County and flows east and south into the Miramichi River at the local service district of Oak Point-Bartibog Bridge.

Geographic entities mentioned:
surface_form: bartibog
instance_of: Watercourse
countries: Canada
coordinates: lat: 47.1086
lon: -65.3707
surface_form: bartibog river
instance_of: Watercourse
countries: Canada
coordinates: lat: 47.1086
lon: -65.3707
The Bartibog River rises in northeastern Northumberland County and flows east and south into the Miramichi River at the local service district of Oak Point-Bartibog Bridge. The Bartibog River watershed is entirely rural, dominated by forests and small farms in the communities of Oak Point-Bartibog Bridge, Lower Newcastle-Russellville, Bartibog, and Bartibog Station.

Geographic entities mentioned:
surface_form: bartibog
instance_of: Watercourse
countries: Canada
coordinates: lat: 47.1086
lon: -65.3707
surface_form: bartibog
instance_of: Watercourse
countries: Canada
coordinates: lat: 47.1086
lon: -65.3707
surface_form: bartibog
instance_of: Watercourse
countries: Canada
coordinates: lat: 47.1086
lon: -65.3707
US and NATO. Geopolitical changes in the Arctic has resulted in a renewed interest from the US due to the Faroe Islands strategic location in the North Atlantic Ocean. In June 2022, an agreement was made between Denmark and the Faroe Islands to set up a NATO air surveillance radar on the mountain Sornfelli in the Faroe Islands.

Geographic entities mentioned:
surface_form: Sornfelli
instance_of: Plateau
countries: Faroe Islands
coordinates: lat: 62.083333333333
lon: -6.8333333333333
Shafter Research Station. Shafter Research Station is an agricultural research station near Shafter, Kern County, California, in the San Joaquin Valley. The station was established in 1922 by the U.S. Department of Agriculture (USDA) as Shafter Cotton Research Station. It was built to provide California with high-quality cotton.

Geographic entities mentioned:
surface_form: San Joaquin Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.628888888889
lon: -120.185
Dakelh territories called Keyoh, include the area along Fraser River (&quot;Lhtakoh&quot; – &quot;rivers within one another&quot;) from north of Prince George (&quot;Lheidli&quot; – &quot;confluence&quot;) to south of Quesnel and including the Barkerville-Wells area, the Nechako Country, the areas around Stuart Lake (&quot;Nak'albun&quot; – &quot;Mount Pope lake&quot;), Trembleur Lake (&quot;Dzinghubun&quot; – &quot;day after lake&quot;), Takla Lake (&quot;Khelhghubun&quot; – &quot;load after lake&quot;), Fraser Lake (&quot;Nadlehbun&quot; – &quot;(fish) run lake&quot;), and Babine Lake, the Bulkley Valley, and the region along the West Road River, west to the Hazelton Mountains and the Kitimat Ranges of the Coast Mountains, including the Kluskus Lakes (&quot;Lhoosk'uz&quot; – &quot;Rocky Mountain whitefish place&quot;), Ootsa Lake (&quot;Oosa Bunk'ut&quot; – &quot;bucket lake&quot;), the Quanchus and Fawnie Ranges, and Cheslatta Lake (&quot;Tsetl'adak Bunk'ut&quot; – &quot;Peak Rock Lake&quot;).

Geographic entities mentioned:
surface_form: Stuart Lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.55
lon: -124.58333333333
surface_form: Trembleur Lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.83
lon: -125.146
surface_form: Takla Lake
instance_of: Lake
countries: Canada
coordinates: lat: 55.31
lon: -125.77
surface_form: Babine Lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.75
lon: -126
surface_form: Bulkley Valley
instance_of: Valley
countries: Canada
coordinates: lat: 54.7819
lon: -127.168
surface_form: Kluskus Lakes
instance_of: Group of lakes
countries: Canada
coordinates: lat: 53.0833
lon: -124.5
surface_form: Cheslatta Lake
instance_of: Lake
countries: Canada
coordinates: lat: 53.7333
lon: -125.35
Farther south, 'Ulkatcho people share the Coast Range with the Coast Salish Nuxalkmc (Bella Coola) and the northern Chilcotin Plateau with Northern Athabaskan speaking strong warrior nation (with political influence from the Similkameen region in the south (of British Columbia), the Pacific coast in the west, and the Rocky Mountains in the east) Tsilhqot'in (Chilkot'in, ᗘᙢᗥᐣ). Culture.

Geographic entities mentioned:
surface_form: Chilcotin Plateau
instance_of: Mountain
countries: Canada
coordinates: lat: 52.166666666666664
lon: -123.41666666666667
Ephialtias pseudena. &quot;Ephialtias pseudena&quot; is a moth of the family Notodontidae. It is found in Panama and the Magdalena Valley of Colombia.

Geographic entities mentioned:
surface_form: Magdalena Valley
instance_of: Valley
countries: Colombia
coordinates: lat: 7.05969444
lon: -73.85308333
He was raised in County Down and maintained a studio at Cushendun, County Antrim. Craig abandoned a career in business, briefly attended the Belfast School of Art, and became a mostly self-taught painter of landscapes. Among his favorite panoramas were County Donegal, Connemara and the Glens of Antrim. Craig was elected to the Royal Ulster Academy and the Royal Hibernian Academy in 1928.

Geographic entities mentioned:
surface_form: Glens of Antrim
instance_of: Valley
countries: United Kingdom
coordinates: lat: 55.16
lon: -6.1
Baltazar Ushca. Baltazar Ushca (12 May 1944 – 11 October 2024) was an Ecuadorian ice harvester. He was perhaps best known for being the last iceman of Chimborazo. Ushca died from injuries suffered after being charged by a bull on 11 October 2024, at the age of 80.

Geographic entities mentioned:
surface_form: Chimborazo
instance_of: Mountain
countries: Ecuador
coordinates: lat: -1.4691666666667
lon: -78.8175
The roots have an ectomycorrhizal association with fungi in the soil. Distribution and habitat. &quot;Microberlinia bisulcata&quot; is endemic to southwestern Cameroon. It is present in Korup National Park, Loum Forest Reserve and on the northern and western foothills of Mount Cameroon. Records from elsewhere are unreliable. It occurs in lowland rainforest, typically in flat sandy areas. Uses.

Geographic entities mentioned:
surface_form: Mount Cameroon
instance_of: Mountain
countries: Cameroon
coordinates: lat: 4.2166666666667
lon: 9.1725
Al-Turtushi was also an accomplished jurist in the Maliki school. Life. ِAbu Bakr was born in Tortosa in 1059 in the northern region of Al-Andalus at the Ebro Delta, at a time when the region had become increasingly fragmented and was divided into various taifa kingdoms. He first traveled to Zaragoza, where he became a student under Abu al-Walid al-Baji, a famous scholar and poet.

Geographic entities mentioned:
surface_form: Ebro Delta
instance_of: Body of water
countries: Spain
coordinates: lat: 40.73243
lon: 0.86964
state of Missouri. It is a tributary of Big Creek. The stream headwaters arise on the south flank of Taum Sauk Mountain at and an elevation of approximately 1220 feet. The stream flows generally east for approximately two miles to its confluence with Big River south of Royal Gorge and adjacent to Missouri routes 72 and 21. The confluence is at and an elevation of 942 feet.

Geographic entities mentioned:
surface_form: Taum Sauk Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.570327777778
lon: -90.7279
History. Shenandoah, originally known as Fair Oaks, was platted in 1870, shortly after the arrival of the Chicago, Burlington and Quincy Railroad into the neighborhood. Its name is derived from the local valley's resemblance to the Shenandoah Valley, in Virginia. In 1885, a smallpox epidemic in Shenandoah prompted the closing of schools, and the cancellation of church services and public meetings.

Geographic entities mentioned:
surface_form: Shenandoah Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.5
lon: -78.85
Life in Chicago. Upon settling in Chicago in 1834, Hubbard purchased a cabin near Lake Michigan from Billy Caldwell and became one of the village's first trustees. Shortly thereafter, Hubbard became the first investor in Gilbert Knapp's claim on the settlement of Port Gilbert, 60 miles north of Chicago, which became the city of Racine, Wisconsin.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
It is a Munro with a height of. It is overshadowed by its neighbour Ben Lui, although it is well seen from the main A82 road. Its name means &quot;mountain of the black rock&quot;, referring to the steep and rocky face on the southwest slopes above Loch Oss, which offer scrambling routes to the summit. Geography and Biology.

Geographic entities mentioned:
surface_form: Ben Lui
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.397004
lon: -4.810525
Its name means &quot;mountain of the black rock&quot;, referring to the steep and rocky face on the southwest slopes above Loch Oss, which offer scrambling routes to the summit. Geography and Biology. Beinn Dubhchraig stands in a group of mountains which rise around the headwaters of the River Cononish and includes two other Munros (Ben Lui and Ben Oss) and the Corbett Beinn Chuirn.

Geographic entities mentioned:
surface_form: Ben Lui
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.397004
lon: -4.810525
surface_form: Ben Oss
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.389272
lon: -4.775488
surface_form: ben oss
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.389272
lon: -4.775488
surface_form: beinn chuirn
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.4236
lon: -4.7883
surface_form: ben lui
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.397004
lon: -4.810525
Beinn Dubhchraig is often climbed in conjunction with some or all of the mountains around the Cononish valley. The view from the summit gives fine views of the mountains of Breadalbane to the west and the twin Munros of Ben More and Stob Binnein are well seen to the south east.

Geographic entities mentioned:
surface_form: Stob Binnein
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.370717
lon: -4.535753
surface_form: ben more
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.424829
lon: -6.014015
surface_form: ben more
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.385952
lon: -4.540087
surface_form: stob binnein
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.370717
lon: -4.535753
The mine workings closed eventually in 1923. Beinn Dubhchraig is linked to the adjacent Munro of Ben Oss, which lies two kilometres to the west, by the Bealach Buidhe which has a height of 779 metres. The ridge down to the bealach is broad and holds a few small lochans within the schist rock hollows. There are corries to both the north and south of the bealach.

Geographic entities mentioned:
surface_form: ben oss
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.389272
lon: -4.775488
The glen of Cononish and the four mountains make up the Ben Lui National Nature Reserve, an area which attracts many biologists who come to study the profusion of mountain plants which grow on the moist rocky cliffs and outcrops. The soil in the reserve is of low acidity and saxifrages grow in abundance. Large herds of deer can be found in the corries around the mountain.

Geographic entities mentioned:
surface_form: ben lui
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.397004
lon: -4.810525
Beinn Dubhchraig. Beinn Dubhchraig () is a mountain in the Scottish Highlands, west of Crianlarich in the northern part of Loch Lomond and the Trossachs National Park. It is a Munro with a height of. It is overshadowed by its neighbour Ben Lui, although it is well seen from the main A82 road.

Geographic entities mentioned:
surface_form: beinn dubhchraig
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.391295
lon: -4.743193
Beinn Dubhchraig. Beinn Dubhchraig () is a mountain in the Scottish Highlands, west of Crianlarich in the northern part of Loch Lomond and the Trossachs National Park. It is a Munro with a height of. It is overshadowed by its neighbour Ben Lui, although it is well seen from the main A82 road.

Geographic entities mentioned:
surface_form: beinn dubhchraig
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.391295
lon: -4.743193
surface_form: loch lomond
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.1482
lon: -4.6515
surface_form: lomond
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.1482
lon: -4.6515
To the north of the bealach is Coire Buidhe which has a very steep headwall which prevents a direct descent from the bealach down to the Cononish valley to the north. To the east, Beinn Dubhchraig falls to the valley of Gleann Auchreoch, much of these lower eastern slopes were planted with conifers in the early 1970s and have become an obstacle to approaches to the mountain from that direction.

Geographic entities mentioned:
surface_form: beinn dubhchraig
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.391295
lon: -4.743193
Frau Hitt. The Frau Hitt () is a peak in the &quot;Nordkette&quot;, the southernmost mountain chain of the Karwendel in Austria. In appearance it resembles a woman (German: &quot;Frau&quot;) on a horse, hence the name. According to legend the peak is a petrified giant queen, called Frau Hitt, who was known for her avarice and self-infatuation. The legend has various versions.

Geographic entities mentioned:
surface_form: Nordkette
instance_of: Mountain
countries: Austria
coordinates: lat: 47.3
lon: 11.35
surface_form: nordkette
instance_of: Mountain
countries: Austria
coordinates: lat: 47.3
lon: 11.35
surface_form: frau hitt
instance_of: Mountain
countries: Austria
coordinates: lat: 47.305278
lon: 11.350556
The Frau Hitt Saddle () lies west of Frau Hitt, where a crossing from the Inn Valley to the Gleirschtal valley is possible (the protected ascent to the Frau Hitt Cirque (&quot;Frau Hitt-Kar&quot;) is north of and below Frau Hitt). Neighbouring crossings are: in the west the &quot;Erl Saddle&quot; near the Solsteinhaus, in the east the Hafelekar top station.

Geographic entities mentioned:
surface_form: Hafelekar
instance_of: Mountain
countries: Austria
coordinates: lat: 47.316667
lon: 11.383333
surface_form: hafelekar
instance_of: Mountain
countries: Austria
coordinates: lat: 47.316667
lon: 11.383333
Frau Hitt. The Frau Hitt () is a peak in the &quot;Nordkette&quot;, the southernmost mountain chain of the Karwendel in Austria. In appearance it resembles a woman (German: &quot;Frau&quot;) on a horse, hence the name. According to legend the peak is a petrified giant queen, called Frau Hitt, who was known for her avarice and self-infatuation. The legend has various versions.

Geographic entities mentioned:
surface_form: frau hitt
instance_of: Mountain
countries: Austria
coordinates: lat: 47.305278
lon: 11.350556