Sarmila/GeoWiki-Features huggingface dataset:
He made multiple returns, but after a few years, the population disappeared. The last confirmed record of the species came in 1935 from near Ooroowilanie, east of Lake Eyre. &quot;Caloprymnus campestris&quot; was well-adapted to the extremely barren and arid regions it inhabited; these traits saved it from competition by introduced species like the European rabbit or domestic sheep.

Geographic entities mentioned:
surface_form: Lake Eyre
instance_of: Lake
countries: Australia
coordinates: lat: -28.406
lon: 137.2963
Piz Nadéls. Piz Nadéls is a mountain of the Swiss Lepontine Alps, located south of Trun in the canton of Graubünden. It lies on the chain between the Val Sumvitg and Val Zavragia. Its steep western face overlooks the Val Nadéls.

Geographic entities mentioned:
surface_form: piz nadéls
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.690083333333
lon: 8.9906111111111
List of the main battles in the history of the Ottoman Empire are shown below. The life span of the empire was more than six centuries, and the maximum territorial extent, at the zenith of its power in the second half of the 16th century, stretched from central Europe to the Persian Gulf and from the Caspian Sea to North Africa. The number of battles the empire fought is quite high.

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
Mount Dulit. Mount Dulit is a mountain in Borneo. It peaks at above sea level and stands at the head of the Baram River in northern Sarawak, Malaysia. It is a western outlier of the Bornean cordillera and is largely covered with montane tropical rainforest.

Geographic entities mentioned:
surface_form: mount dulit
instance_of: Mountain
countries: Malaysia
coordinates: lat: 3.33333333
lon: 114.15
Prince Edward Glacier. Prince Edward Glacier () is a glacier draining the north side of Cotton Plateau in the Queen Elizabeth Range and flowing north for about 6 nautical miles (11 km) along the west side of Hochstein Ridge. Named by New Zealand Antarctic Place-Names Committee (NZ-APC) for Prince Edward, Duke of Edinburgh, son of Elizabeth II of the United Kingdom.

Geographic entities mentioned:
surface_form: Cotton Plateau
instance_of: Plateau
coordinates: lat: -82.9
lon: 159.667
surface_form: Hochstein Ridge
instance_of: Mountain
coordinates: lat: -82.75
lon: 159.78333333
Indian River (West Canada Creek tributary). Indian River starts at Spruce Lake and flows into West Canada Creek in Herkimer County, New York.

Geographic entities mentioned:
surface_form: Spruce Lake
instance_of: Lake
countries: United States
coordinates: lat: 43.533333333333
lon: -74.611666666667
Kvutzat Alon. Kvutzat Alon () is an Israeli kibbutz. Located in the Jezreel Valley in northern Israel, it falls under the jurisdiction of the Jezreel Valley Regional Council. As of 2022, it had a population of 781. History. Kvutzat Alon was founded in August 1948 as a kvutza, by a group of Polish Jews from Łódź, who immigrated to Israel, many of whom were Holocaust survivors.

Geographic entities mentioned:
surface_form: Jezreel Valley
instance_of: Valley
countries: Israel
coordinates: lat: 32.596388888889
lon: 35.241944444444
Flagstone Peak () is located in the Wind River Range in the U.S. state of Wyoming. The peak is the 12th highest peak in Wyoming. The summit is located on the Continental Divide and is in both Shoshone and Bridger-Teton National Forests. The Flagstone Peak-Southeast Peak () lies to the southeast. Hazards. Encountering bears is a concern in the Wind River Range.

Geographic entities mentioned:
surface_form: shoshone
instance_of: Lake
countries: United States
coordinates: lat: 44.3722
lon: -110.713
Flagstone Peak (Fremont County, Wyoming). Flagstone Peak () is located in the Wind River Range in the U.S. state of Wyoming. The peak is the 12th highest peak in Wyoming. The summit is located on the Continental Divide and is in both Shoshone and Bridger-Teton National Forests. The Flagstone Peak-Southeast Peak () lies to the southeast. Hazards.

Geographic entities mentioned:
surface_form: flagstone peak (fremont county, wyoming)
instance_of: Mountain
countries: United States
coordinates: lat: 43.2153
lon: -109.676
Flagstone Peak (Fremont County, Wyoming). Flagstone Peak () is located in the Wind River Range in the U.S. state of Wyoming. The peak is the 12th highest peak in Wyoming. The summit is located on the Continental Divide and is in both Shoshone and Bridger-Teton National Forests. The Flagstone Peak-Southeast Peak () lies to the southeast. Hazards.

Geographic entities mentioned:
surface_form: flagstone peak
instance_of: Mountain
countries: United States
coordinates: lat: 43.2153
lon: -109.676
Flagstone Peak () is located in the Wind River Range in the U.S. state of Wyoming. The peak is the 12th highest peak in Wyoming. The summit is located on the Continental Divide and is in both Shoshone and Bridger-Teton National Forests. The Flagstone Peak-Southeast Peak () lies to the southeast. Hazards. Encountering bears is a concern in the Wind River Range.

Geographic entities mentioned:
surface_form: flagstone peak
instance_of: Mountain
countries: United States
coordinates: lat: 43.2153
lon: -109.676
It was transferred from the dissolved Skaraborg County to Jönköping County in 1998. Geography. Things to do in the municipality include activities related to the lake Vättern, such as fishing, bathing and hiking. It offers plenty of nature and outdoor activities.

Geographic entities mentioned:
surface_form: Vättern
instance_of: Lake
countries: Sweden
coordinates: lat: 58.4
lon: 14.6
Many of the first Tongan Americans came to the United States in connection to the Church of Jesus Christ of Latter-day Saints. They have strong presence in parts of Salt Lake Valley in Utah, especially West Valley City and Salt Lake City. Utah is roughly one percent Tongan, a high rate compared to Tongans only making up less than a scant 0.02% of the US population.

Geographic entities mentioned:
surface_form: Salt Lake Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.6839
lon: -111.978
The viewpoints of Mather Point, (and Yavapai Point), look northwards (across Granite Gorge), up Bright Angel Canyon, and view the prominences that align it, especially the nearest of Isis Temple and Cheops Pyramid, and on the east, Zoroaster Temple, with Demaray Point, Bradley Point, and Sumner Butte.

Geographic entities mentioned:
surface_form: Isis Temple
instance_of: Mountain
countries: United States
coordinates: lat: 36.1408
lon: -112.138
surface_form: Cheops Pyramid
instance_of: Landform
countries: United States
coordinates: lat: 36.11804
lon: -112.12211
Abdul Karim Amrullah (born as Muhammad Rasul; 10 February 1879 – 2 June 1945), known as Haji Rasul, was a Muslim reformer who led reformation of Islam in Sumatra, Dutch East Indies (now Indonesia). Personal life. Haji Rasul was born in Sungai Batang, Maninjau, West Sumatra on February 10, 1879. His father was Muslim ulema, Syekh Muhammad Amrullah Tuanku Kisai and his mother Andung Tarawas.

Geographic entities mentioned:
surface_form: Maninjau
instance_of: Lake
countries: Indonesia
coordinates: lat: -0.31666666666667
lon: 100.2
In the Ojibwe language it is called &quot;Ozaagi-ziibi&quot;, meaning &quot;River of the Sauks&quot;. It issues from Lake Osakis on the Todd County / Stearns County line. During times of low water in Lake Osakis, water can be diverted into the lake across the divide from the Long Prairie River, joining the watershed of the Sauk River with that of the Crow Wing River.

Geographic entities mentioned:
surface_form: Lake Osakis
instance_of: Lake
countries: United States
coordinates: lat: 45.8967
lon: -95.1222
Poco Mandasawu. Poco Mandasawu is a lava dome of Ranakah located in the south-central part of the island of Flores, Indonesia. It is the highest point of the island.

Geographic entities mentioned:
surface_form: Ranakah
instance_of: Mountain
countries: Indonesia
coordinates: lat: -8.63664
lon: 120.53095
surface_form: poco mandasawu
instance_of: Mountain
countries: Indonesia
coordinates: lat: -8.65
lon: 120.45
Poco Mandasawu. Poco Mandasawu is a lava dome of Ranakah located in the south-central part of the island of Flores, Indonesia. It is the highest point of the island.

Geographic entities mentioned:
surface_form: poco mandasawu
instance_of: Mountain
countries: Indonesia
coordinates: lat: -8.65
lon: 120.45
The work contributed toward understanding of intracontinental subduction zones. She has extensive field experience spanning California (Mojave desert, Coachella Valley, Klamath Mountains); Betic Cordillera in southern Spain; Syros Island in Greece; Rio Grande in New Mexico; Kenai Peninsula in Alaska; Northeastern China; Morocco in Northern Africa. Awards and recognition.

Geographic entities mentioned:
surface_form: Coachella Valley
instance_of: Valley
countries: United States
coordinates: lat: 33.72
lon: -116.2
Misema Caldera. The Misema Caldera is a 2,704-2,707 million year old caldera in Ontario and Quebec, Canada. Geographic extent. It is the caldera that forms the Blake River Megacaldera Complex and has a diameter of 40-80 kilometres. Composition. The caldera is also a coalescence of at least two large mafic shield volcanoes that formed more than 2703 million years ago.

Geographic entities mentioned:
surface_form: misema caldera
instance_of: Mountain
countries: Canada
coordinates: lat: 48.39
lon: -79.45
Composition. The caldera is also a coalescence of at least two large mafic shield volcanoes that formed more than 2703 million years ago. The rim of the Misema Caldera contains a 10-15 kilometre wide inner and outer ring zone, in which many mafic ring dike complexes and subaqueous pyroclastic sediments are detected.

Geographic entities mentioned:
surface_form: misema caldera
instance_of: Mountain
countries: Canada
coordinates: lat: 48.39
lon: -79.45
The mafic ring dike structures may be deeper level expressions of summit calderas related to a shield volcano phase while the pyroclastic fragments could either be associated with satellite cones or the result of Misema caldera collapse. Misema Caldera is the oldest and largest caldera associated with the Blake River Megacaldera Complex and is comparable in size to Lake Toba caldera in Indonesia.

Geographic entities mentioned:
surface_form: misema caldera
instance_of: Mountain
countries: Canada
coordinates: lat: 48.39
lon: -79.45
Course. The official beginning of the Klamath River is at Lake Ewauna, a small natural lake near Klamath Falls, Oregon. The primary inflow of Lake Ewauna is the short Link River, which connects it to Upper Klamath Lake. Upper Klamath, in turn, is fed by the Williamson River (originating in the Winema National Forest) and Wood River (originating in Crater Lake National Park).

Geographic entities mentioned:
surface_form: Lake Ewauna
instance_of: Lake
countries: United States
coordinates: lat: 42.213330555556
lon: -121.77861111111
Course. The official beginning of the Klamath River is at Lake Ewauna, a small natural lake near Klamath Falls, Oregon. The primary inflow of Lake Ewauna is the short Link River, which connects it to Upper Klamath Lake. Upper Klamath, in turn, is fed by the Williamson River (originating in the Winema National Forest) and Wood River (originating in Crater Lake National Park).

Geographic entities mentioned:
surface_form: Upper Klamath Lake
instance_of: Lake
countries: United States
coordinates: lat: 42.392222222222
lon: -121.88027777778
For the first below Lake Ewauna, the Klamath River takes a slow meandering course through what was formerly the Klamath Marshes, which were drained for agriculture in the early 20th century. An artificial channel diverts water from the Lost River, which normally flows into Tule Lake, into the Klamath during periods of high runoff.

Geographic entities mentioned:
surface_form: Tule Lake
instance_of: Lake
countries: United States
coordinates: lat: 41.909322222222
lon: -121.53304722222
Most of the Upper Klamath Basin is in Oregon, with some parts extending south into California. Situated between the Cascades and the Oregon high desert and northwest of the Modoc Plateau, it features a semi-arid climate and is characterized by large, flat alluvial valleys separated by long mountain ridges. Elevations range from in the valleys to in the Cascades.

Geographic entities mentioned:
surface_form: Modoc Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 41.6
lon: -121.2
Although many streams flowing into Upper Klamath Lake derive their flow from snowmelt, its largest sources – the Williamson and Wood Rivers – are predominantly fed by large springs. Upper and Lower Klamath Lakes and Tule Lake were once part of of connected wetlands, over three-quarters of which have been drained for agriculture.

Geographic entities mentioned:
surface_form: Tule Lake
instance_of: Lake
countries: United States
coordinates: lat: 41.909322222222
lon: -121.53304722222
Since the 20th century, the Lost River and Lower Klamath Lake basins – as well as the neighboring Butte Valley–Meiss Lake basin – have been artificially altered to discharge floodwaters into the Klamath River via diversion dams and drainage facilities.

Geographic entities mentioned:
surface_form: Meiss Lake
instance_of: Lake
countries: United States
coordinates: lat: 41.860291666667
lon: -122.05801944444
About 88 percent of the Klamath River's total flow originates in the Lower Basin, even though it only accounts for 62 percent of the land area. The Trinity River is the largest sub-basin of the Lower Klamath; the main stem originates in the Trinity Alps west of Redding, while the South Fork Trinity River's origin at North Yolla Bolly Mountain is the southernmost point in the entire Klamath Basin.

Geographic entities mentioned:
surface_form: North Yolla Bolly Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.19611111
lon: -122.97361111
Yreka and Montague are located within Shasta Valley. To the west is the smaller Scott Valley, which includes the towns of Fort Jones, Etna, Greenview and Callahan. Hayfork Valley and the community of Hayfork are located in Trinity County, while Hoopa Valley and the surrounding Hoopa Reservation are on the Trinity River in Humboldt County. Tributaries and sub-basins.

Geographic entities mentioned:
surface_form: Scott Valley
instance_of: Valley
countries: United States
coordinates: lat: 41.5541
lon: -122.8552
Starting in 1963, these works directed about per year out of the Trinity River, representing about one-tenth of the total runoff of the Klamath-Trinity River system. Trinity River water was a key factor in the development of the Westlands Water District, today one of the most productive agricultural areas in California, on the west side of the San Joaquin Valley.

Geographic entities mentioned:
surface_form: San Joaquin Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.628888888889
lon: -120.185
In 1847 he went to North America as traveling geologist for the &quot;Jardin des Plantes&quot;, charged with studying the United States and the English possessions in North America. The next year, he joined Agassiz in Boston, and accompanied him to the Lake Superior region, visiting the copper mines of the Keweenaw Peninsula, Lake Huron, and Niagara.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
It was described by Alessandro Guiggi, an Italian botanist. Distribution and ecology. &quot;Opuntia mantaroensis&quot; primarily grows in the Mantaro Valley (Río Mantaro Valley), Huancavelica, Peru, where scattered individuals and localities have been identified. Its range is within the dry-tropical zone of Peru, where it grows in-between other species of prickly pear cactus.

Geographic entities mentioned:
surface_form: Mantaro Valley (Río Mantaro Valley)
instance_of: Valley
countries: Peru
coordinates: lat: -11.91666667
lon: -75.33333333
The entire last rig heist scene was filmed along Domenigoni Parkway on the southern side of San Jacinto/Hemet in the San Jacinto Valley near Diamond Valley Lake. Before filming, both Jordana Brewster and Michelle Rodriguez did not have driver's licenses, so they took driving lessons during production.

Geographic entities mentioned:
surface_form: San Jacinto Valley
instance_of: Valley
countries: United States
coordinates: lat: 33.7978
lon: -117.005
In March 2021 he was succeeded by Sir Charles Hobhouse. Private life. Truluck married Jennifer J. Bell in Wensleydale in 1976. They have one son and one daughter, and live in the Chalke Valley, having previously lived near Amesbury, Swindon, and Salisbury, all in Wiltshire.

Geographic entities mentioned:
surface_form: Wensleydale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.3056
lon: -2.16667
Great Trossachs Path. The Great Trossachs Path is a long-distance footpath through the Trossachs, in the Stirling council area of Scotland. It runs between Callander in the east and Inversnaid on the banks of Loch Lomond in the west, passing along the northern shores of Loch Katrine and Loch Arklet.

Geographic entities mentioned:
surface_form: Loch Lomond
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.1482
lon: -4.6515
surface_form: Loch Katrine
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.254444444444445
lon: -4.515555555555555
Produced by Irwin Allen, the screenplay by Carl Foreman and Stirling Silliphant is loosely based on the 1969 novel &quot;The Day the World Ended&quot; by Gordon Thomas and Max Morgan-Witts detailing the factual 1902 volcanic eruption of Mount Pelée on Martinique, which killed 30,000 people in five minutes by pyroclastic flow.

Geographic entities mentioned:
surface_form: Mount Pelée
instance_of: Mountain
countries: France
coordinates: lat: 14.813055555556
lon: -61.165555555556
Development. &quot;The Day the World Ended&quot;, by English television writers Gordon Thomas and Max Morgan-Witts, was a 1969 non-fiction account of the disastrous eruption of Mount Pelée in Martinique in 1902, which killed 30,000 people. It was called &quot;literally impossible to put down&quot; by &quot;The New York Times&quot;. Film rights were bought by Irwin Allen.

Geographic entities mentioned:
surface_form: Mount Pelée
instance_of: Mountain
countries: France
coordinates: lat: 14.813055555556
lon: -61.165555555556
Pasca. Pasca is a town and municipality in the Cundinamarca department of Colombia located in the Andes. It belongs to the Sumapaz Province. Pasca is situated on the Altiplano Cundiboyacense at a distance of from the capital Bogotá. It borders Fusagasugá, Sibaté and Soacha in the north, Bogotá D.C. in the north and east, Arbeláez in the south and Fusagasugá in the west.

Geographic entities mentioned:
surface_form: Altiplano Cundiboyacense
instance_of: Plateau
countries: Colombia
coordinates: lat: 5.532209
lon: -73.362877
Fresno, California. Fresno (;) is a city in the San Joaquin Valley of California, United States. It is the county seat of Fresno County and the largest city in the greater Central Valley region, as well as the most populated city in Central California.

Geographic entities mentioned:
surface_form: San Joaquin Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.628888888889
lon: -120.185
History. The original inhabitants of the San Joaquin Valley region were the Yokuts people and Miwok people, who engaged in trading with other Californian tribes of Native Americans including coastal peoples such as the Chumash of the Central California coast, with whom they are thought to have traded plant and animal products.

Geographic entities mentioned:
surface_form: San Joaquin Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.628888888889
lon: -120.185
Just south of Yosemite National Park, it is the nearest major city to the park. Likewise, Sierra National Forest is, Kings Canyon National Park is and Sequoia National Park is. The city is located near several Sierra Nevada lakes including Bass Lake, Shaver Lake, and Huntington Lake. Fresno is also only two and a half hours from Monterey, Carmel, Big Sur and the central coast.

Geographic entities mentioned:
surface_form: Shaver Lake
instance_of: Lake
countries: United States
coordinates: lat: 37.125969444444
lon: -119.29075
Economy. Fresno is the center of Metropolitan Fresno and serves as the regional hub for the San Joaquin Valley and the greater Central Valley region. The unincorporated area and rural cities surrounding Fresno remain predominantly tied to large-scale agricultural production. In 1958, Fresno was selected by Bank of America to first launch the BankAmericard credit card, which was later renamed Visa.

Geographic entities mentioned:
surface_form: San Joaquin Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.628888888889
lon: -120.185
Marindahl Lake. Marindahl Lake is a lake in Yankton County, South Dakota. It is located 4 miles west and 3 miles south of the city of Irene.

Geographic entities mentioned:
surface_form: marindahl lake
instance_of: Lake
countries: United States
coordinates: lat: 43.0454736
lon: -97.2596415
Wila Willk'i (Pando). Wila Willk'i (Aymara &quot;wila&quot; blood, blood-red, &quot;willk'i&quot; gap, &quot;red gap&quot;, also spelled &quot;Wila Willqui, Wila Wilqui&quot;) is a mountain in the Andes of Bolivia. It is located at the Peruvian border in the La Paz Department, José Manuel Pando Province, Catacora Municipality, southwest of T'ula Qullu.

Geographic entities mentioned:
surface_form: T'ula Qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.2667
lon: -69.5667
surface_form: t'ula qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.67777778
lon: -65.76666667
surface_form: t'ula qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.2667
lon: -69.5667
Wila Willk'i (Pando). Wila Willk'i (Aymara &quot;wila&quot; blood, blood-red, &quot;willk'i&quot; gap, &quot;red gap&quot;, also spelled &quot;Wila Willqui, Wila Wilqui&quot;) is a mountain in the Andes of Bolivia. It is located at the Peruvian border in the La Paz Department, José Manuel Pando Province, Catacora Municipality, southwest of T'ula Qullu.

Geographic entities mentioned:
surface_form: wila willk'i
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.8967
lon: -66.6217
surface_form: willk'i
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.39861111
lon: -69.02222222
surface_form: wila willk'i
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.28388889
lon: -69.635
surface_form: wila willk'i
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.0117
lon: -67.4608
Wila Willk'i (Pando). Wila Willk'i (Aymara &quot;wila&quot; blood, blood-red, &quot;willk'i&quot; gap, &quot;red gap&quot;, also spelled &quot;Wila Willqui, Wila Wilqui&quot;) is a mountain in the Andes of Bolivia. It is located at the Peruvian border in the La Paz Department, José Manuel Pando Province, Catacora Municipality, southwest of T'ula Qullu.

Geographic entities mentioned:
surface_form: wila willk'i
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.8967
lon: -66.6217
surface_form: willk'i
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.39861111
lon: -69.02222222
surface_form: willk'i
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.39861111
lon: -69.02222222
surface_form: wila willk'i
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.28388889
lon: -69.635
surface_form: wila willk'i
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.0117
lon: -67.4608
Cime di Caronella. Cime di Caronella is a mountain of Lombardy, Italy. It is located within the Bergamo Alps.

Geographic entities mentioned:
surface_form: cime di caronella
instance_of: Mountain
countries: Italy
coordinates: lat: 46.09055556
lon: 10.09055556
In 1624/25, he immigrated to the Mughal realm, where he became acquainted with the young governor of Kabul, Mirza Ahsan-Allah Zafar Khan. The latter also wrote poetry, and became the main patron of Saib, who became his teacher in poetry. Saib accompanied Zafar Khan and his father on military campaigns in the Deccan Plateau, before returning to Isfahan in 1632. Return to Iran.

Geographic entities mentioned:
surface_form: Deccan Plateau
instance_of: Plateau
countries: India
coordinates: lat: 15
lon: 77
zolii&quot; is known from five localities widely scattered across northern Africa. It is known in Libya from the Oasis of Elbarkat (Al Barkat) 8 km south of Ghat in Fezzan and from near Ajedabia in western Cyrenaica. In Egypt it is known from Wadi El Natrun; this subpopulation was previously misidentified as belonging to &quot;P. intermedius&quot;. This account follows Trape &quot;et al&quot;.

Geographic entities mentioned:
surface_form: Wadi El Natrun
instance_of: Valley
countries: Egypt
coordinates: lat: 30.416666666667
lon: 30.333333333333
Individuals were found restricted to semi-desert areas with grassy vegetation on sandy soil or other steppe vegetation near oases. The best known subpopulation is located in Wadi El Natrun/Egypt at the margin of salt marshes. Here it can be found climbing in microhabitats created by the halfa grass &quot;Desmostachya bipinnata&quot; and also in stands of &quot;Alhagi graecorum&quot;.

Geographic entities mentioned:
surface_form: Wadi El Natrun
instance_of: Valley
countries: Egypt
coordinates: lat: 30.416666666667
lon: 30.333333333333
Taweh Creek. Taweh Creek is a tributary of Mess Creek, which in turn is a tributary of the Stikine River in northwest part of the province of British Columbia, Canada. It flows generally northwest for about to join Mess Creek about northwest of Mess Creek's confluence with Raspberry Creek. Taweh Creek's watershed covers and its mean annual discharge is estimated at.

Geographic entities mentioned:
surface_form: Mess Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.88296
lon: -131.2206
surface_form: taweh creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.71638
lon: -130.97063
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
Taweh Creek is in Mount Edziza Provincial Park which lies within the traditional territory of the Tahltan people. Geography. Taweh Creek originates on the southern end of the Big Raven Plateau. From its source just south of Mount Edziza between Coffee Crater and Cartoona Peak, Taweh Creek flows about southwest to the northern base of Keda Cone.

Geographic entities mentioned:
surface_form: Big Raven Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.7167
lon: -130.75
surface_form: taweh creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.71638
lon: -130.97063
Geography. Taweh Creek originates on the southern end of the Big Raven Plateau. From its source just south of Mount Edziza between Coffee Crater and Cartoona Peak, Taweh Creek flows about southwest to the northern base of Keda Cone. It then flows about west to near the southwestern end of the Big Raven Plateau.

Geographic entities mentioned:
surface_form: Mount Edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: Coffee Crater
instance_of: Mountain
countries: Canada
coordinates: lat: 57.63
lon: -130.67
surface_form: Cartoona Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.6067
lon: -130.615
surface_form: taweh creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.71638
lon: -130.97063
Taweh Creek then flows about west through a gorge to empty into Mess Creek. Taweh Creek's only named tributary, Sezill Creek, is about east of Taweh Creek's confluence with Mess Creek. It is about long and flows northwest into Taweh Creek from the western side of Mount Edziza. Geology. Taweh Creek flows from a linear group of volcanoes called the Mount Edziza volcanic complex.

Geographic entities mentioned:
surface_form: Sezill Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.69967
lon: -130.88724
surface_form: taweh creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.71638
lon: -130.97063
surface_form: taweh creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.71638
lon: -130.97063
surface_form: mess creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.88296
lon: -131.2206
It is about long and flows northwest into Taweh Creek from the western side of Mount Edziza. Geology. Taweh Creek flows from a linear group of volcanoes called the Mount Edziza volcanic complex. As a result, Taweh Creek has been engulfed by tongues of lava from the neighbouring Snowshoe Lava Field.

Geographic entities mentioned:
surface_form: Mount Edziza volcanic complex
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5
lon: -130.6
surface_form: taweh creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.71638
lon: -130.97063
It was built to serve the nearly Yukon Telegraph Line which was constructed by the Dominion Government Telegraph Service between 1897 and 1901 to send messages from Ashcroft, British Columbia in the south to Dawson City, Yukon in the north. The telegraph trail crosses other tributaries along the eastern side of Mess Creek, including Crayke Creek about north of Taweh Creek.

Geographic entities mentioned:
surface_form: Crayke Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.73298
lon: -130.97063
surface_form: taweh creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.71638
lon: -130.97063
surface_form: mess creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.88296
lon: -131.2206
Taweh Creek. Taweh Creek is a tributary of Mess Creek, which in turn is a tributary of the Stikine River in northwest part of the province of British Columbia, Canada. It flows generally northwest for about to join Mess Creek about northwest of Mess Creek's confluence with Raspberry Creek. Taweh Creek's watershed covers and its mean annual discharge is estimated at.

Geographic entities mentioned:
surface_form: taweh creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.71638
lon: -130.97063
It flows generally northwest for about to join Mess Creek about northwest of Mess Creek's confluence with Raspberry Creek. Taweh Creek's watershed covers and its mean annual discharge is estimated at. The mouth of Taweh Creek is located about southeast of Telegraph Creek, about west-southwest of Iskut and about southwest of Dease Lake.

Geographic entities mentioned:
surface_form: taweh creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.71638
lon: -130.97063
Taweh Creek's watershed covers and its mean annual discharge is estimated at. The mouth of Taweh Creek is located about southeast of Telegraph Creek, about west-southwest of Iskut and about southwest of Dease Lake. Taweh Creek's watershed's land cover is classified as 41.3% barren, 21.1% shrubland, 20.7% conifer forest, 8.4% herbaceous, 8.1% snow/glacier, and small amounts of other cover.

Geographic entities mentioned:
surface_form: taweh creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.71638
lon: -130.97063
Taweh Creek's watershed's land cover is classified as 41.3% barren, 21.1% shrubland, 20.7% conifer forest, 8.4% herbaceous, 8.1% snow/glacier, and small amounts of other cover. Taweh Creek is in Mount Edziza Provincial Park which lies within the traditional territory of the Tahltan people. Geography. Taweh Creek originates on the southern end of the Big Raven Plateau.

Geographic entities mentioned:
surface_form: taweh creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.71638
lon: -130.97063
It then flows about west to near the southwestern end of the Big Raven Plateau. From there, Taweh Creek flows about northwest to Hola Bluff where it flows north-northwest through a valley on the eastern edge of the Big Raven Plateau for an additional. Taweh Creek then flows about west through a gorge to empty into Mess Creek.

Geographic entities mentioned:
surface_form: taweh creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.71638
lon: -130.97063
From there, Taweh Creek flows about northwest to Hola Bluff where it flows north-northwest through a valley on the eastern edge of the Big Raven Plateau for an additional. Taweh Creek then flows about west through a gorge to empty into Mess Creek. Taweh Creek's only named tributary, Sezill Creek, is about east of Taweh Creek's confluence with Mess Creek.

Geographic entities mentioned:
surface_form: taweh creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.71638
lon: -130.97063
surface_form: mess creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.88296
lon: -131.2206
Taweh Creek then flows about west through a gorge to empty into Mess Creek. Taweh Creek's only named tributary, Sezill Creek, is about east of Taweh Creek's confluence with Mess Creek. It is about long and flows northwest into Taweh Creek from the western side of Mount Edziza. Geology. Taweh Creek flows from a linear group of volcanoes called the Mount Edziza volcanic complex.

Geographic entities mentioned:
surface_form: taweh creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.71638
lon: -130.97063
Geology. Taweh Creek flows from a linear group of volcanoes called the Mount Edziza volcanic complex. As a result, Taweh Creek has been engulfed by tongues of lava from the neighbouring Snowshoe Lava Field. Most of this lava issued from cinder cones but one of the youngest lava flows to enter Taweh Creek originated from a fissure vent known as The Saucer.

Geographic entities mentioned:
surface_form: taweh creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.71638
lon: -130.97063
As a result, Taweh Creek has been engulfed by tongues of lava from the neighbouring Snowshoe Lava Field. Most of this lava issued from cinder cones but one of the youngest lava flows to enter Taweh Creek originated from a fissure vent known as The Saucer. While the majority of this lava converged into the head of Taweh Creek, some of it formerly extended more than downstream to near Mess Creek.

Geographic entities mentioned:
surface_form: taweh creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.71638
lon: -130.97063
Most of this lava issued from cinder cones but one of the youngest lava flows to enter Taweh Creek originated from a fissure vent known as The Saucer. While the majority of this lava converged into the head of Taweh Creek, some of it formerly extended more than downstream to near Mess Creek. An erosional remnant of this lava forms the lip of an waterfall at an elevation of.

Geographic entities mentioned:
surface_form: taweh creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.71638
lon: -130.97063
surface_form: mess creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.88296
lon: -131.2206
While the majority of this lava converged into the head of Taweh Creek, some of it formerly extended more than downstream to near Mess Creek. An erosional remnant of this lava forms the lip of an waterfall at an elevation of. The Taweh Creek lava flows are of Holocene age and form part of the Big Raven Formation. History. The historic Yukon Telegraph Trail crosses Taweh Creek in Mess Creek valley.

Geographic entities mentioned:
surface_form: taweh creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.71638
lon: -130.97063
History. The historic Yukon Telegraph Trail crosses Taweh Creek in Mess Creek valley. It was built to serve the nearly Yukon Telegraph Line which was constructed by the Dominion Government Telegraph Service between 1897 and 1901 to send messages from Ashcroft, British Columbia in the south to Dawson City, Yukon in the north.

Geographic entities mentioned:
surface_form: taweh creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.71638
lon: -130.97063
surface_form: mess creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.88296
lon: -131.2206
The telegraph trail crosses other tributaries along the eastern side of Mess Creek, including Crayke Creek about north of Taweh Creek. Taweh Creek was formerly called Big Sheep Creek which appeared on a BC Lands map published in 1929. Its current name was suggested by the BC Geographic Division to avoid confusion with other similarly-named features; it first appeared on maps in 1945.

Geographic entities mentioned:
surface_form: taweh creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.71638
lon: -130.97063
Taweh Creek. Taweh Creek is a tributary of Mess Creek, which in turn is a tributary of the Stikine River in northwest part of the province of British Columbia, Canada. It flows generally northwest for about to join Mess Creek about northwest of Mess Creek's confluence with Raspberry Creek. Taweh Creek's watershed covers and its mean annual discharge is estimated at.

Geographic entities mentioned:
surface_form: mess creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.88296
lon: -131.2206
surface_form: mess creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.88296
lon: -131.2206
History. The historic Yukon Telegraph Trail crosses Taweh Creek in Mess Creek valley. It was built to serve the nearly Yukon Telegraph Line which was constructed by the Dominion Government Telegraph Service between 1897 and 1901 to send messages from Ashcroft, British Columbia in the south to Dawson City, Yukon in the north.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
Other filming locations, simulating the desert, were Buttercup Valley in the Algodones Dunes, California, and Pilot Knob Mesa, California. The flying sequences were all filmed at Pilot Knob Mesa near Winterhaven, located in California's Imperial Valley, on the western fringes of Yuma, Arizona. Aircraft used.

Geographic entities mentioned:
surface_form: Imperial Valley
instance_of: Valley
countries: United States
coordinates: lat: 33.1
lon: -115.5
There is a sea for each for the four cardinal directions. The West Sea is Qinghai Lake, the East Sea is the East China Sea, the North Sea is Lake Baikal, and the South Sea is the South China Sea. Two of the seas were symbolic until they were tied to genuine locations during the Han dynasty's wars with the Xiongnu.

Geographic entities mentioned:
surface_form: Qinghai Lake
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 37
lon: 100
surface_form: Lake Baikal
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.30277778
lon: 108.00472222
Only two of the Four Seas were tied to real locations, the East Sea with the East China Sea and the South Sea with the South China Sea. During the Han dynasty, wars with the Xiongnu brought them north to Lake Baikal. They recorded that the lake was a &quot;huge sea&quot; (hanhai) and designated it the mythical North Sea.

Geographic entities mentioned:
surface_form: Lake Baikal
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.30277778
lon: 108.00472222
They recorded that the lake was a &quot;huge sea&quot; (hanhai) and designated it the mythical North Sea. They also encountered Qinghai Lake, which they called the West Sea, and the lakes Lop Nur and Bostang in Xinjiang. The Han dynasty expanded beyond the traditional West Sea and reached Lake Balkhash, the westernmost boundary of the empire and the new West Sea of the dynasty.

Geographic entities mentioned:
surface_form: Qinghai Lake
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 37
lon: 100
They also encountered Qinghai Lake, which they called the West Sea, and the lakes Lop Nur and Bostang in Xinjiang. The Han dynasty expanded beyond the traditional West Sea and reached Lake Balkhash, the westernmost boundary of the empire and the new West Sea of the dynasty. Expeditions were sent to explore the Persian Gulf, but went no further.

Geographic entities mentioned:
surface_form: Lake Balkhash
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 46.540833333333
lon: 74.878888888889
Geography. The limestone mountain rises above the karst fields, in which there are many caves. One of the largest caves is the Quartet mine (-340 m). The highest point in the vicinity is Mount Agepsta northwest of mountain Achibakhi. Flora. Mixed forest and subalpine (tree line) endemic flora grow on the mountain.

Geographic entities mentioned:
surface_form: Mount Agepsta
instance_of: Mountain
countries: Georgia
Russia
Russian Empire
Soviet Union
coordinates: lat: 43.548333333333
lon: 40.480555555556
Achibakh Mountain. Achibakh or Achibakhi () is a mountain in Abkhazia. Height 2376 m. The highest peak of the plateau Rykhva. On the map of Abkhazia, issued in 2009 by the Geographical Society of Abkhazia, the mountain is called Arttara. Geography. The limestone mountain rises above the karst fields, in which there are many caves. One of the largest caves is the Quartet mine (-340 m).

Geographic entities mentioned:
surface_form: achibakh mountain
instance_of: Mountain
countries: Georgia
coordinates: lat: 43.418024
lon: 40.581597
Joan Mary Hore was born in Bedford, England, on 12 August 1890, to Edward Coode Hore who was a missionary, explorer, mariner and shipbuilder and his wife Annie née Boyle. Both were associated with the London Missionary Society (LMS). Joan had one sibling, Jack (b. 1882) who was the first white child to visit Lake Tanganyika. Jack fell ill and he died in London (April 1889).

Geographic entities mentioned:
surface_form: Lake Tanganyika
instance_of: Lake
countries: Tanzania
Democratic Republic of the Congo
Burundi
Zambia
coordinates: lat: -6.1
lon: 29.5
Migori County. Migori County is a county in the former Nyanza Province of southwestern Kenya. It borders Homa Bay County to the north, Kisii County to the northeast, Narok County to the southeast, Tanzania to the west and south, and Lake Victoria to the west. The county also borders Uganda via Migingo Island in Lake Victoria. The county's headquarter is Migori, which is also its largest town.

Geographic entities mentioned:
surface_form: Lake Victoria
instance_of: Lake
countries: Tanzania
Uganda
Kenya
coordinates: lat: -1
lon: 33
Location. Migori Town (-1.0634,34.4731) is 368 kilometers from Nairobi. Migori town is bordered by hills. Water bodies in the county include the Kuja and Migori rivers, and Lake Victoria. Economy. The main economic activities include agriculture, fishing, manufacturing and mining. There is some small scale gold mining carried out in the county.

Geographic entities mentioned:
surface_form: Lake Victoria
instance_of: Lake
countries: Tanzania
Uganda
Kenya
coordinates: lat: -1
lon: 33
Star of Oregon (event). The Star of Oregon episode of American history began in 1840 and ended in 1843. This enterprise by pioneers in the Willamette Valley of present-day Oregon consisted of building a ship they named &quot;Star of Oregon&quot; and then sailing it to California in order to bring back cattle to Oregon Country.

Geographic entities mentioned:
surface_form: Willamette Valley
instance_of: Valley
countries: United States
coordinates: lat: 44.9
lon: -123.1
Once spring came and the crew gathered at Cash Creek there were now a total of 42 people ready to head north to Oregon Country. This party started north with 1,250 head of cattle, 600 horses and mules, and 3,000 sheep. The journey overland took 75 days, and in mid-May 1843, they arrived back in the Willamette Valley of the Oregon Country. Legacy.

Geographic entities mentioned:
surface_form: Willamette Valley
instance_of: Valley
countries: United States
coordinates: lat: 44.9
lon: -123.1
It's believed that the destruction of the pyramid started at the end of the New Kingdom at the latest, and was particularly intense during the Roman and early Christian eras when a Coptic monastery was built in nearby Wadi Karin. It has been proven, moreover, that at the end of the nineteenth century, stone was still being hauled away at the rate of three hundred camel loads a day.

Geographic entities mentioned:
surface_form: Wadi Karin
instance_of: Valley
countries: Egypt
coordinates: lat: 30.416666666667
lon: 30.333333333333
The story about the horse named Vesleblakken is based upon a childhood memory from the author's upbringing in Rendalen. The story was first published in &quot;Skisser&quot; (1891). His other novels and stories often described folk life in the valley of Østerdalen. He also wrote historical novels, contemporary novels and poetry. In 1911, Bull became a Knight 1st grade in the Order of St. Olav.

Geographic entities mentioned:
surface_form: Østerdalen
instance_of: Valley
countries: Norway
coordinates: lat: 61.575916666666664
lon: 11.087111111111112
Mount Rio Branco. Mount Rio Branco () is a mountain, 975 m, standing 2.5 nautical miles (4.6 km) east of Cape Perez on the west coast of Graham Land. Discovered by the French Antarctic Expedition, 1908–10, and named by Charcot for José Paranhos, Baron of Rio Branco, at that time Minister of Foreign Affairs of Brazil.

Geographic entities mentioned:
surface_form: mount rio branco
instance_of: Mountain
coordinates: lat: -65.4167
lon: -64
surface_form: rio branco
instance_of: Mountain
coordinates: lat: -65.4167
lon: -64
Mount Rio Branco. Mount Rio Branco () is a mountain, 975 m, standing 2.5 nautical miles (4.6 km) east of Cape Perez on the west coast of Graham Land. Discovered by the French Antarctic Expedition, 1908–10, and named by Charcot for José Paranhos, Baron of Rio Branco, at that time Minister of Foreign Affairs of Brazil.

Geographic entities mentioned:
surface_form: rio branco
instance_of: Mountain
coordinates: lat: -65.4167
lon: -64
Najafgarh is situated Southwest of the New Delhi City Centre and northwest to the district headquarters at Dwarka. It has an average elevation of above mean Sea Level. Najafgarh Drain, the continuation of the Sahibi River and an elongation of the Najafgarh Lake is the Indian capital's most polluted body of water due to the direct inflow of untreated sewage from surrounding populated areas.

Geographic entities mentioned:
surface_form: Najafgarh Lake
instance_of: Lake
countries: India
coordinates: lat: 28.504
lon: 76.944
The commission instead issued their collective notes. The notes were referred to as the &quot;ploughman series&quot; because they an image of a ploughman ploughing a field with a horse-drawn plough. The notes, which were denominated in notes for £1, £5, £10, £20, £50 and £100, used as the back images a collection of images of Ireland, in order the Custom House, Dublin, St.

Geographic entities mentioned:
surface_form: Croagh Patrick
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.7595
lon: -9.6584
In 1162 Emperor Xiaozong of Song posthumously dissolved his unjust charges and rehabilitated his honours. For their part in Yue's death, iron statues of Qin Hui, Lady Wang, and two of Qin's subordinates, Moqi Xie () and Zhang Jun (), were made to kneel before Yue Fei's tomb near West Lake in Hangzhou. For centuries, these statues were cursed, spat on, and urinated upon by people.

Geographic entities mentioned:
surface_form: West Lake
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 30.2375
lon: 120.14083333333
Whales in Vermont. Fossils of marine invertebrates found in the Champlain Valley reveal that Vermont was underwater during the Paleozoic Era, more than 300 million years ago, long before the advent of mammals. In recent geologic history, the last glacier melted away about 12,500 years ago, and the sea poured in.

Geographic entities mentioned:
surface_form: Champlain Valley
instance_of: Valley
countries: United States
coordinates: lat: 44.45868
lon: -73.42617