Sarmila/GeoWiki-Features huggingface dataset:
Thracian tomb Shushmanets. The Thracian tomb at Shushmanets is a mound located in the Valley of the Thracian Rulers. It was built as a temple in the 4th century BC and later used as a tomb. Architecture. The temple has a long and wide entry corridor and an antechamber, a semi-cylindrical room supported by an elegant column. The top of this column has the form of a knucklebone.

Geographic entities mentioned:
surface_form: Valley of the Thracian Rulers
instance_of: Valley
countries: Bulgaria
coordinates: lat: 42.6906192
lon: 25.380075
They are also carved from a single piece of wood. Apart from the specimens from Tanzania, these features can also be found on stools made by the Tabwa and Bemba people, who live west of Lake Tanganyika in the Democratic Republic of the Congo and in Zambia. Such similarities in sculptures from different ethnic groups are attributed to migratory movements and the exchange of goods, e.g.

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
[...] For these farmers and hunters with a their lose relationship to nature, a few details are enough to recognise a self-contained, independent reality in a block of wood that appears to us to have hardly been worked on at all...&quot; Also, Meur points out that &quot;Homo habilis&quot; first appeared in the vicinity of the great lakes of Central Africa, where the first evidence of art in the form of rock paintings has been found.

Geographic entities mentioned:
surface_form: great lakes of Central Africa
instance_of: Group of lakes
countries: Burundi
Zambia
Kenya
Democratic Republic of the Congo
Malawi
Mozambique
Rwanda
Tanzania
Uganda
Ethiopia
coordinates: lat: -8
lon: 35
It is native to the western United States from central Washington to northeastern California, where it grows in moist to wet, sandy habitat types, such as playas (dry lakes). It is not a common plant; it is known from about fifteen occurrences in the Modoc Plateau region of California, it is a candidate for protection in Oregon, and it is state-listed as a threatened species in Washington.

Geographic entities mentioned:
surface_form: Modoc Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 41.6
lon: -121.2
Etzel (mountain). The Etzel is a mountain on the south side of Lake Zürich in Switzerland. Although its elevation, of, is relatively modest, it is notable for its aspect when viewed from the lake and its surroundings. It is also well known for its views over Lake Zurich (including the Seedamm near Rapperswil) and Lake Sihl and over the Prealps and Alps. There is a mountain inn at the summit.

Geographic entities mentioned:
surface_form: Lake Sihl
instance_of: Lake
countries: Switzerland
coordinates: lat: 47.116666666667
lon: 8.7833333333333
surface_form: lake zurich
instance_of: Lake
countries: Switzerland
coordinates: lat: 47.2475
lon: 8.6775
Etzel (mountain). The Etzel is a mountain on the south side of Lake Zürich in Switzerland. Although its elevation, of, is relatively modest, it is notable for its aspect when viewed from the lake and its surroundings. It is also well known for its views over Lake Zurich (including the Seedamm near Rapperswil) and Lake Sihl and over the Prealps and Alps. There is a mountain inn at the summit.

Geographic entities mentioned:
surface_form: etzel
instance_of: Mountain
countries: Switzerland
coordinates: lat: 47.1778
lon: 8.7675
Etzel (mountain). The Etzel is a mountain on the south side of Lake Zürich in Switzerland. Although its elevation, of, is relatively modest, it is notable for its aspect when viewed from the lake and its surroundings. It is also well known for its views over Lake Zurich (including the Seedamm near Rapperswil) and Lake Sihl and over the Prealps and Alps. There is a mountain inn at the summit.

Geographic entities mentioned:
surface_form: etzel
instance_of: Mountain
countries: Switzerland
coordinates: lat: 47.1778
lon: 8.7675
surface_form: lake zürich
instance_of: Lake
countries: Switzerland
coordinates: lat: 47.2475
lon: 8.6775
There is a mountain inn at the summit. The mountain forms part of the Schwyzer Alps mountain range, and lies in the canton of Schwyz. Its summit and slopes are divided between the municipalities of Feusisberg, which lies to the north, and Einsiedeln, which lies to the south. The mountain has given its name to the 1934-built MV &quot;Etzel&quot;, now preserved on Lake Zürich.

Geographic entities mentioned:
surface_form: etzel
instance_of: Mountain
countries: Switzerland
coordinates: lat: 47.1778
lon: 8.7675
surface_form: lake zürich
instance_of: Lake
countries: Switzerland
coordinates: lat: 47.2475
lon: 8.6775
Steward is a partner in the Sloan Digital Sky Survey-III, which is located in New Mexico at Apache Point Observatory. Steward used to maintain a student observatory on Tumamoc Hill approximately west of the campus, but that is no longer in operation. The original observatory dome in Tucson now houses the Ray White Jr. 21-inch telescope and is used for public outreach and undergraduate education.

Geographic entities mentioned:
surface_form: Tumamoc Hill
instance_of: Landform
countries: United States
coordinates: lat: 32.2141
lon: -111.006
The Mara mobile veterinary unit covers the Masai Mara National Reserve, the adjacent Mara Triangle, neighbouring community areas, as well as the Lake Naivasha and Nakuru areas within the Rift Valley; when needed, the unit also operates as far west as Ruma National Park and Lake Victoria.

Geographic entities mentioned:
surface_form: Lake Naivasha
instance_of: Lake
countries: Kenya
coordinates: lat: -0.76852777777778
lon: 36.350644444444
surface_form: Lake Victoria
instance_of: Lake
countries: Tanzania
Uganda
Kenya
coordinates: lat: -1
lon: 33
The Amboseli mobile veterinary unit operates out of Amboseli National Park and services the Southern Conservation Area encompassing Kajiado, Namanga, Magadi, Lake Natron as well as the Southern Tsavo West area including Lake Jipe, an ecosystem famous for large number of elephants.

Geographic entities mentioned:
surface_form: Lake Jipe
instance_of: Lake
countries: Tanzania
Kenya
coordinates: lat: -3.6069444444444
lon: 37.761666666667
Tropical storm force winds were reported, peaking at at Shell Beach, Louisiana, on the south shore of Lake Borgne. At the same location, tides between above normal were measured. Four people were rescued by the United States Coast Guard after their tugboat sank in Lake Pontchartrain, while three others swam to shore. Additionally, two fatalities occurred in the vicinity of Mobile, Alabama.

Geographic entities mentioned:
surface_form: Lake Pontchartrain
instance_of: Lake
countries: United States
coordinates: lat: 30.188888888889
lon: -90.101388888889
Overlooking Lake Michigan, it was founded in 1920, and soon became one of Chicago's landmark hotels and a longtime rival of the Palmer House.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Design and construction. The Olmsted Brothers of Brookline, Massachusetts, were selected to plan the Exposition; the firm was already involved in planning parks and parkways for the City of Seattle. John C. Olmsted visited Seattle in October 1906 and saw the dominant form of Mount Rainier toward the southeast. He selected the mountain as the focus of the primary axis of the Exposition.

Geographic entities mentioned:
surface_form: Mount Rainier
instance_of: Mountain
countries: United States
coordinates: lat: 46.85166666666667
lon: -121.76027777777777
Hogback (New York). Hogback is a mountain in Schoharie County, New York. It is located northeast of Cobleskill. Barrack Zourie is located northwest and Mount Shank is located southwest of Hogback.

Geographic entities mentioned:
surface_form: Barrack Zourie
instance_of: Mountain
countries: United States
coordinates: lat: 42.725277777778
lon: -74.490277777778
surface_form: Mount Shank
instance_of: Mountain
countries: United States
coordinates: lat: 42.68313
lon: -74.49875
surface_form: hogback
instance_of: Mountain
countries: United States
coordinates: lat: 42.706388888889
lon: -74.465
Hogback (New York). Hogback is a mountain in Schoharie County, New York. It is located northeast of Cobleskill. Barrack Zourie is located northwest and Mount Shank is located southwest of Hogback.

Geographic entities mentioned:
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: hogback
instance_of: Mountain
countries: United States
coordinates: lat: 42.706388888889
lon: -74.465
Hogback (New York). Hogback is a mountain in Schoharie County, New York. It is located northeast of Cobleskill. Barrack Zourie is located northwest and Mount Shank is located southwest of Hogback.

Geographic entities mentioned:
surface_form: hogback (new york)
instance_of: Mountain
countries: United States
coordinates: lat: 42.706388888889
lon: -74.465
It is a major left tributary of the Zeravshan. The Fan Darya is formed at the confluence of the rivers Yaghnob, which flows west from the Yaghnob Valley, and the Iskander Darya, which has its source in Lake Iskanderkul and flows east. Both the Yaghnob and the Iskander Darya drain the valleys between the Zeravshan Range to the north, the Gissar Range to the south and the Fan Mountains to the west.

Geographic entities mentioned:
surface_form: Yaghnob Valley
instance_of: Valley
countries: Tajikistan
coordinates: lat: 39.2
lon: 69
surface_form: Lake Iskanderkul
instance_of: Lake
countries: Tajikistan
coordinates: lat: 39.074444444444
lon: 68.368333333333
Lake Lysimachia. Lysimachia () is a lake in Aetolia-Acarnania, western Greece. Its area is 13.2 km2, its depth is around 9 m. It is fed by the small river Ermitsa, and by a canal that connects the lake with the larger Lake Trichonida to its east. Its outflow is the river Dimikos, which drains into the river Acheloos. The city of Agrinio lies 6 km to the northeast.

Geographic entities mentioned:
surface_form: Lake Trichonida
instance_of: Lake
countries: Greece
coordinates: lat: 38.5725
lon: 21.5525
surface_form: trichonida
instance_of: Lake
countries: Greece
coordinates: lat: 38.5725
lon: 21.5525
Lake Lysimachia. Lysimachia () is a lake in Aetolia-Acarnania, western Greece. Its area is 13.2 km2, its depth is around 9 m. It is fed by the small river Ermitsa, and by a canal that connects the lake with the larger Lake Trichonida to its east. Its outflow is the river Dimikos, which drains into the river Acheloos. The city of Agrinio lies 6 km to the northeast.

Geographic entities mentioned:
surface_form: lake lysimachia
instance_of: Lake
countries: Greece
coordinates: lat: 38.56666667
lon: 21.36388889
surface_form: lysimachia
instance_of: Lake
countries: Greece
coordinates: lat: 38.56666667
lon: 21.36388889
Lake Lysimachia. Lysimachia () is a lake in Aetolia-Acarnania, western Greece. Its area is 13.2 km2, its depth is around 9 m. It is fed by the small river Ermitsa, and by a canal that connects the lake with the larger Lake Trichonida to its east. Its outflow is the river Dimikos, which drains into the river Acheloos. The city of Agrinio lies 6 km to the northeast.

Geographic entities mentioned:
surface_form: lysimachia
instance_of: Lake
countries: Greece
coordinates: lat: 38.56666667
lon: 21.36388889
Per Aru. The Per Aru is a river in Northern Province, Sri Lanka. The river rises in northern Vavuniya District, before flowing north/north-east through Vavuniya District and Mullaitivu District. The river empties into Nanthi Kadal lagoon.

Geographic entities mentioned:
surface_form: per aru
instance_of: Watercourse
countries: Sri Lanka
Per Aru. The Per Aru is a river in Northern Province, Sri Lanka. The river rises in northern Vavuniya District, before flowing north/north-east through Vavuniya District and Mullaitivu District. The river empties into Nanthi Kadal lagoon.

Geographic entities mentioned:
surface_form: nanthi kadal
instance_of: Lake
countries: Sri Lanka
coordinates: lat: 9.2833333333333
lon: 80.766666666667
Mount Franklin (Victoria). Mount Franklin (Djadjawurrung: &quot;Willambeparamal&quot;) is an extinct volcano about 10 km north of Daylesford and 4.6 km south east of Franklinford in Victoria, Australia. A road spirals round the outside slopes covered with pine trees, into a flat 50 acre caldera, and onto the rim which hosts a fire lookout, parking area and picnic ground.

Geographic entities mentioned:
surface_form: mount franklin (victoria)
instance_of: Mountain
countries: Australia
coordinates: lat: -37.2651
lon: 144.15
surface_form: mount franklin
instance_of: Mountain
countries: Australia
coordinates: lat: -35.4872
lon: 148.774
Mount Franklin (Victoria). Mount Franklin (Djadjawurrung: &quot;Willambeparamal&quot;) is an extinct volcano about 10 km north of Daylesford and 4.6 km south east of Franklinford in Victoria, Australia. A road spirals round the outside slopes covered with pine trees, into a flat 50 acre caldera, and onto the rim which hosts a fire lookout, parking area and picnic ground.

Geographic entities mentioned:
surface_form: mount franklin
instance_of: Mountain
countries: Australia
coordinates: lat: -37.2651
lon: 144.15
surface_form: mount franklin
instance_of: Mountain
countries: Australia
coordinates: lat: -35.4872
lon: 148.774
There is space for tents, and to park caravans and RVs. A toilet block and water tank (non-potable) is located close to the entrance. Being a prominent local landmark within Hepburn Shire, the mountain is included within the boundaries of the Mount Franklin Reserve managed by Parks Victoria. History. The mountain was created by a volcanic eruption about 470,000 years ago.

Geographic entities mentioned:
surface_form: mount franklin
instance_of: Mountain
countries: Australia
coordinates: lat: -37.2651
lon: 144.15
surface_form: mount franklin
instance_of: Mountain
countries: Australia
coordinates: lat: -35.4872
lon: 148.774
The volcanic eruptions may have been witnessed by members of the Dja Dja Wurrung native Aboriginal tribe who called this country the ‘smoking grounds’. The clan that occupied the country around Mount Franklin were the Gunangara Gundidj who called it &quot;Willambeparamal&quot; meaning &quot;home of the emus&quot;.

Geographic entities mentioned:
surface_form: mount franklin
instance_of: Mountain
countries: Australia
coordinates: lat: -37.2651
lon: 144.15
surface_form: mount franklin
instance_of: Mountain
countries: Australia
coordinates: lat: -37.2651
lon: 144.15
surface_form: mount franklin
instance_of: Mountain
countries: Australia
coordinates: lat: -35.4872
lon: 148.774
surface_form: mount franklin
instance_of: Mountain
countries: Australia
coordinates: lat: -35.4872
lon: 148.774
Both ethnographical and archaeological evidence indicates that frequent large ceremonial gatherings took place in the area. Lava from Mount Franklin and other volcanoes in the area filled valleys and buried the gold bearing streams that became the renowned ‘deep leads’ of the gold mining era.

Geographic entities mentioned:
surface_form: mount franklin
instance_of: Mountain
countries: Australia
coordinates: lat: -37.2651
lon: 144.15
surface_form: mount franklin
instance_of: Mountain
countries: Australia
coordinates: lat: -35.4872
lon: 148.774
Charles Joseph La Trobe, superintendent of the Port Phillip District of New South Wales named the mountain after Sir John Franklin after they climbed the hill together in December 1843. In 1840, in response to concerns about the treatment of Aboriginal people by the settlers, the government took over Mount Franklin and the surrounding area for the Loddon Aboriginal Protectorate Station.

Geographic entities mentioned:
surface_form: mount franklin
instance_of: Mountain
countries: Australia
coordinates: lat: -37.2651
lon: 144.15
surface_form: mount franklin
instance_of: Mountain
countries: Australia
coordinates: lat: -35.4872
lon: 148.774
This placed additional pressures on the protectorate station and it was reduced and finally relocated. Around 1865 the presence of a deep lead in Mount Franklin was established. Deep lead mining was initially unsuccessful, and it was not until the late 1870s that the Franklinford Gold Mining Company mined at Mount Franklin on a significant scale.

Geographic entities mentioned:
surface_form: mount franklin
instance_of: Mountain
countries: Australia
coordinates: lat: -37.2651
lon: 144.15
surface_form: mount franklin
instance_of: Mountain
countries: Australia
coordinates: lat: -37.2651
lon: 144.15
surface_form: mount franklin
instance_of: Mountain
countries: Australia
coordinates: lat: -35.4872
lon: 148.774
surface_form: mount franklin
instance_of: Mountain
countries: Australia
coordinates: lat: -35.4872
lon: 148.774
This gold was created by lava flows during the Newer Volcanic period, were mined intensively during the nineteenth century. One such company operated a mining lease at the eastern foot of Mount Franklin. In 1866, the crater of Mount Franklin was set aside as a recreation reserve, and the remainder reserved as State forest.

Geographic entities mentioned:
surface_form: mount franklin
instance_of: Mountain
countries: Australia
coordinates: lat: -37.2651
lon: 144.15
surface_form: mount franklin
instance_of: Mountain
countries: Australia
coordinates: lat: -37.2651
lon: 144.15
surface_form: mount franklin
instance_of: Mountain
countries: Australia
coordinates: lat: -35.4872
lon: 148.774
surface_form: mount franklin
instance_of: Mountain
countries: Australia
coordinates: lat: -35.4872
lon: 148.774
Owing to the high demand for land in the district, two areas of the reserve were excised and sold for agricultural settlement. This galvanised popular support for the permanent reservation of Mount Franklin. During the 1870s and 80s, scenic qualities of natural bushland gained popularity as recreational venues as compared to formal parks and gardens.

Geographic entities mentioned:
surface_form: mount franklin
instance_of: Mountain
countries: Australia
coordinates: lat: -37.2651
lon: 144.15
surface_form: mount franklin
instance_of: Mountain
countries: Australia
coordinates: lat: -35.4872
lon: 148.774
During the 1870s and 80s, scenic qualities of natural bushland gained popularity as recreational venues as compared to formal parks and gardens. In 1875, a meeting asked the Victorian government to reserve all the land at Mount Franklin for public purposes and a reservation of 157 acres was gazetted the following year under shared management of the surrounding local government areas.

Geographic entities mentioned:
surface_form: mount franklin
instance_of: Mountain
countries: Australia
coordinates: lat: -37.2651
lon: 144.15
surface_form: mount franklin
instance_of: Mountain
countries: Australia
coordinates: lat: -37.2651
lon: 144.15
surface_form: mount franklin
instance_of: Mountain
countries: Australia
coordinates: lat: -35.4872
lon: 148.774
surface_form: mount franklin
instance_of: Mountain
countries: Australia
coordinates: lat: -35.4872
lon: 148.774
Mount Franklin was promoted as a local beauty spot within easy reach of Daylesford and Hepburn Springs mineral springs resort. A shelter shed and rainwater tank were erected. In 1880, the railway network was extended to Daylesford making destinations like Mount Franklin a comfortable day-trip from Melbourne. In 1944, a devastating bushfire destroyed most of the native vegetation on the mount.

Geographic entities mentioned:
surface_form: mount franklin
instance_of: Mountain
countries: Australia
coordinates: lat: -37.2651
lon: 144.15
surface_form: mount franklin
instance_of: Mountain
countries: Australia
coordinates: lat: -35.4872
lon: 148.774
In 1972, the Department of Crown Lands and Survey took over the committee of management. In 1977, Mount Franklin was included in the new Hepburn Regional Park and managed by the Forest Commission of Victoria. 'Mount Franklin' mineral spring.

Geographic entities mentioned:
surface_form: mount franklin
instance_of: Mountain
countries: Australia
coordinates: lat: -37.2651
lon: 144.15
surface_form: mount franklin
instance_of: Mountain
countries: Australia
coordinates: lat: -35.4872
lon: 148.774
Ordovician rocks outcrop within a few chains of the spring. The more calcareous parts of the spring deposit were formerly burnt for lime and old kilns remain on the flat&quot;
Coca Cola, which had a licence to extract 35 megalitres, renamed the spring ‘Mount Franklin’ as part of a re-branding exercise. Their peak per annum extraction was over 15 ML and the total to around 1986 was 14.52 ML.

Geographic entities mentioned:
surface_form: mount franklin
instance_of: Mountain
countries: Australia
coordinates: lat: -37.2651
lon: 144.15
surface_form: mount franklin
instance_of: Mountain
countries: Australia
coordinates: lat: -37.2651
lon: 144.15
surface_form: mount franklin
instance_of: Mountain
countries: Australia
coordinates: lat: -35.4872
lon: 148.774
surface_form: mount franklin
instance_of: Mountain
countries: Australia
coordinates: lat: -35.4872
lon: 148.774
Meals are generally rich in carbohydrates, and vegetables are almost always cooked in coconut milk; meat recipes include pochero, adobo, tapa and dinuguan. Commonly eaten fish are mackerel and anchovy; in Lake Buhi, the sinarapan or &quot;tabyos&quot; (known as the smallest fish in the world) is common. Livelihood. Copra processing and abacá stripping are generally done by hand.

Geographic entities mentioned:
surface_form: Lake Buhi
instance_of: Lake
countries: Philippines
coordinates: lat: 13.45
lon: 123.51666666667
In short, the film is about how the road trip becomes a Paathasala of sorts and prepares them for the big journey called life. Production. The film is a road based film and 95% of the film was shot outdoors at Gandikota, the Godavari River, Horsley Hills, Hyderabad and the villages near Kadapa. Soundtrack. The music for the film was composed by Rahul Raj with lyrics by Sri Mani.

Geographic entities mentioned:
surface_form: Horsley Hills
instance_of: Mountain
countries: India
coordinates: lat: 13.6508702
lon: 78.3965255
They are partially bounded by the Ottawa, St. Lawrence, and Saguenay River. The Laurentian Mountains reside in the Laurentian Upland, which extends as far west as Lake Huron, with foothills extending into northeastern Ontario. Sub-ranges in the upland are the Opeongo Hills, Misquah Hills, Huron Mountains, and the Porcupine Mountains.

Geographic entities mentioned:
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
The Laurentian Mountains reside in the Laurentian Upland, which extends as far west as Lake Huron, with foothills extending into northeastern Ontario. Sub-ranges in the upland are the Opeongo Hills, Misquah Hills, Huron Mountains, and the Porcupine Mountains. This region is extensively forested and contains nearly untouched wilderness, with it not being suited for agriculture.

Geographic entities mentioned:
surface_form: Opeongo Hills
instance_of: Mountain
countries: Canada
coordinates: lat: 45.5
lon: -77.67
surface_form: Misquah Hills
instance_of: Landform
countries: United States
coordinates: lat: 47.98
lon: -90.56
It is close to the major cities of Kobe and Osaka, and is part of the Kansai region. Okuike is located on a height of approximately 500–600 meters above sea level on the Southern aspect, and is located towards the Eastern part of Mount Rokkō (六甲山, Rokkō-san). The &quot;village&quot; of Okuike is home to around 730 properties and is often referred to as the &quot;Beverly Hills of Japan&quot;.

Geographic entities mentioned:
surface_form: Mount Rokkō
instance_of: Mountain
countries: Japan
coordinates: lat: 34.777777777778
lon: 135.26388888889
The altitude of Okuike allows it to have far reaching views, sometimes of 100 kilometers (or more) across Osaka Bay, towards the Nara prefecture, the Kii Mountains (Mount Hakkyō 1,914 meters), the Wakayama prefecture, Awajishima, Shikoku, Kansai International Airport, Osaka, Kobe, the Akashi Kaikyō Bridge (明石海峡大橋, Akashi Kaikyō Ōhashi) and the Seto Inland Sea National Park.

Geographic entities mentioned:
surface_form: Mount Hakkyō
instance_of: Mountain
countries: Japan
coordinates: lat: 34.173611
lon: 135.9075
2021 ICF Canoe Sprint World Championships – Men's VL2. The men's VL2 competition at the 2021 ICF Canoe Sprint World Championships in Copenhagen took place on Lake Bagsværd. Schedule. All times are Central European Summer Time (UTC+2)
Heats. The fastest three boats in each heat advanced directly to the final.

Geographic entities mentioned:
surface_form: Lake Bagsværd
instance_of: Lake
countries: Denmark
coordinates: lat: 55.772222222222
lon: 12.458333333333
Severe rainstorms can also cause sewers to overflow into lakes and rivers, which can threaten beach safety and drinking water supplies. For example, heavy rains in August 2014 led to nearly 10 billion gallons of sewer overflows in southeastern Michigan, much of which ended up in Lake St. Clair and eventually Lake Erie.

Geographic entities mentioned:
surface_form: Lake St. Clair
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.450265
lon: -82.67572
Clair and eventually Lake Erie. More severe rainstorms could also cause sewers in Milwaukee and Chicago to overflow into Lake Michigan more often, which could pollute beaches in Michigan&quot;. &quot;One advantage of climate change is that warmer winters reduce the number of days that ice prevents navigation.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
She describes herself as &quot;on a mission to make science and space exploration disruptively accessible.&quot;
Ariel Waldman is the director of “Antarctica Unearthed”, a nature documentary about the McMurdo Dry Valleys, which she filmed entirely solo without a film crew during her two month expedition as a researcher with the McMurdo Dry Valleys LTER team.

Geographic entities mentioned:
surface_form: McMurdo Dry Valleys
instance_of: Valley
coordinates: lat: -77.466666666667
lon: 162.51666666667
Little Harbour (Gander Lake). xjeq42vymbn6m0n47onn7ezq6k90b" xml:space="preserve">Little Harbour is a small unattended recreation area situated on Gander Lake, near Gander, Newfoundland. Access to this area is via a 1.5 kilometre gravel road from Route 1 (the Trans-Canada Highway). Little Harbour is a recreational park used by residents of Gander for boating and picnicking.

Geographic entities mentioned:
surface_form: Gander Lake
instance_of: Lake
countries: Canada
coordinates: lat: 48.931111111111
lon: -54.734166666667
Geography. The Blue Mountains include several mountain ranges, from the Ochoco Mountains and Maury Mountains in the west near Prineville, Oregon, through the Greenhorn Mountains, the Aldrich Mountains, and the Strawberry Range, to the Elkhorn Mountains. The tallest peaks are Rock Creek Butte at in the Elkhorn Mountains, and Strawberry Mountain at in the Strawberry Range.

Geographic entities mentioned:
surface_form: Rock Creek Butte
instance_of: Mountain
countries: United States
coordinates: lat: 44.816666666667
lon: -118.10361111111
During westward expansion of the United States. In the mid-1800s, the Blue Mountains were a formidable obstacle to settlers traveling on the Oregon Trail and were often the last mountain range American pioneers had to cross before either reaching southeast Washington near Walla Walla or passing down the Columbia River Gorge to the end of the Oregon Trail in the Willamette Valley near Oregon City.

Geographic entities mentioned:
surface_form: Willamette Valley
instance_of: Valley
countries: United States
coordinates: lat: 44.9
lon: -123.1
The fold belt is mainly argillite, with thick amphibolite in the Jinja area and basal arenite in some locations. Parts of the belt are granitized, with low-grade phyllite close to Lake Victoria. Overall, the metamorphic grade tends to decrease southwards.

Geographic entities mentioned:
surface_form: Lake Victoria
instance_of: Lake
countries: Tanzania
Uganda
Kenya
coordinates: lat: -1
lon: 33
An arcuate suite of dykes were emplaced around 1,370 million years ago within the largely Neoarchaean and Palaeoproterozoic rocks from Kampala westwards. The Mityana Group of sandstones and conglomerates occur around Lake Wamala and nearby Mityana as well as forming the larger part of the Ssese Islands in Lake Victoria. Neoproterozoic (1 billion - 539 million years ago).

Geographic entities mentioned:
surface_form: Lake Wamala
instance_of: Lake
countries: Uganda
coordinates: lat: 0.32833333333333
lon: 31.840555555556
Its entire outcrop is thrust-bound except where overlain by Cenozoic volcanics. Similar rocks occupy the country northeast of a line through Pader and Kitgum to form the Akur Massif whilst a third klippe forms the Morungole Massif to the northeast. These klippen are intruded by a suite of granites, charnockites and similar rocks dating from around 680 to 740 million years ago. Paleozoic.

Geographic entities mentioned:
surface_form: Morungole Massif
instance_of: Mountain
countries: Uganda
coordinates: lat: 3.8166666666667
lon: 34.033333333333
Cenozoic (66 million years ago – present). Several volcanic centres in the east of the country were active during the Cenozoic. The carbonatites and nephelinites, lavas and agglomerates together with lahar deposits are collectively referred to as the Elgon Complex after Mount Elgon, the principal eruptive centre.

Geographic entities mentioned:
surface_form: Mount Elgon
instance_of: Mountain
countries: Uganda
Kenya
coordinates: lat: 1.1185
lon: 34.5265
Structural geology and tectonics. Structurally, the geology of Uganda is strongly influenced by fold belts and shear zones, as well as the East Africa Rift related crustal downwarping in the Pleistocene that formed Lake Victoria. The Aswa Shear Zone is one example of several Neoproterozoic shear zones in Precambrian rocks, running for 300 kilometers on a northwestern trend.

Geographic entities mentioned:
surface_form: Lake Victoria
instance_of: Lake
countries: Tanzania
Uganda
Kenya
coordinates: lat: -1
lon: 33
The East Africa Rift defines the western border of Uganda with the Democratic Republic of the Congo. The rift is occupied by Lake Albert, Lake Edward and Lake George, along with the horst block of the Ruwenzori Mountains. Modern sediment depths in the Rift Valley are believed by 1.8 to 4 kilometers. Although volcanoes are no longer active in Uganda, the country has some remnant hot springs.

Geographic entities mentioned:
surface_form: Lake Edward
instance_of: Lake
countries: Uganda
Democratic Republic of the Congo
coordinates: lat: -0.33333333333333
lon: 29.6
Biography. Stamatios Kapsas was born in the village of Pazarakia (now Kryopigi, Chalkidiki) in the late 18th century. At an early age he moved to Sykia to find work, but quickly came into conflict with the local Ottoman authorities, and became a klepht active in the region of Sithonia, Mount Cholomon, and the Chasikochoria (modern Polygyros area).

Geographic entities mentioned:
surface_form: Mount Cholomon
instance_of: Mountain
countries: Greece
coordinates: lat: 40.45944444444444
lon: 23.52027777777778
By the time of the outbreak of the Greek War of Independence in 1821, he was &quot;serdar&quot; (watchman) of the central administrative body of the monasteries of Mount Athos at Karyes. On 23 March 1821, with the aid of ship captains from Psara and Ainos, Emmanouil Pappas landed on Athos with guns and ammunition. After meeting with Kapsas, they began forming an army.

Geographic entities mentioned:
surface_form: Mount Athos
instance_of: Mountain
countries: Greece
coordinates: lat: 40.15833333333333
lon: 24.327222222222222
Mount Dama Ali. Mount Dama Ali is a wide shield volcano in Ethiopia, on the shore of Lake Abbe.

Geographic entities mentioned:
surface_form: mount dama ali
instance_of: Mountain
countries: Ethiopia
coordinates: lat: 11.28724
lon: 41.63811
surface_form: dama ali
instance_of: Mountain
countries: Ethiopia
coordinates: lat: 11.28724
lon: 41.63811
Miguel Buiza died from lung cancer while in exile in Marseille, on 23 June 1963, barely a year after his arrival from Algeria, without having been able to return to Seville, the city of his birth. He is buried at the graveyard in Hyères, in the Var department. Less than two months after Miguel Buiza's death his widow published a short obituary in the Spanish ABC newspaper.

Geographic entities mentioned:
surface_form: Hyères
instance_of: Mountain
countries: France
coordinates: lat: 43.118888888889
lon: 6.1286111111111
Petrie Ice Rises. Petrie Ice Rises () is a group of ice rises extending in a north-south line, lying merged within the Wilkins Ice Shelf, to the west of Alexander Island, Antarctica. The group was seen from the air on a British Antarctic Survey (BAS) radio echo sounding flight around Alexander Island on 11 February 1967 and was later accurately positioned from US Landsat imagery.

Geographic entities mentioned:
surface_form: petrie ice rises
instance_of: Landform
coordinates: lat: -70.55
lon: -72.2
Petrie Ice Rises. Petrie Ice Rises () is a group of ice rises extending in a north-south line, lying merged within the Wilkins Ice Shelf, to the west of Alexander Island, Antarctica. The group was seen from the air on a British Antarctic Survey (BAS) radio echo sounding flight around Alexander Island on 11 February 1967 and was later accurately positioned from US Landsat imagery.

Geographic entities mentioned:
surface_form: petrie ice rises
instance_of: Landform
coordinates: lat: -70.55
lon: -72.2
surface_form: alexander
instance_of: Mountain
coordinates: lat: -63.3039
lon: -55.80564
It was named by the United Kingdom Antarctic Place-Names Committee in 1980 after David L. Petrie, a BAS and Scott Polar Research Institute electronics technician (from about 1966–1970), who was on the flight.

Geographic entities mentioned:
surface_form: scott
instance_of: Mountain
coordinates: lat: -65.15158
lon: -64.04798
Petrie Ice Rises. Petrie Ice Rises () is a group of ice rises extending in a north-south line, lying merged within the Wilkins Ice Shelf, to the west of Alexander Island, Antarctica. The group was seen from the air on a British Antarctic Survey (BAS) radio echo sounding flight around Alexander Island on 11 February 1967 and was later accurately positioned from US Landsat imagery.

Geographic entities mentioned:
surface_form: alexander
instance_of: Mountain
coordinates: lat: -63.3039
lon: -55.80564
In the spring of 1851, he joined the Oregon Indian Commission (composed of John P. Gaines, Alonzo A. Skinner and Beverly S. Allen) on a treaty excursion, traveling through the Willamette Valley negotiating with the tribes, passing through Oregon City and again ending up in Fort Vancouver in July, 1851.

Geographic entities mentioned:
surface_form: Willamette Valley
instance_of: Valley
countries: United States
coordinates: lat: 44.9
lon: -123.1
Tule Lake is a seasonal lake that forms in the winter when Scotts Creek overflows its banks. The lake floods every year except when there is a severe drought. It drains along Scotts Creek into Rodman Slough, which flows into Clear Lake. There is only a slight change in elevation along Scotts Creek between Blue Lakes, Tule Lake and Clear Lake, and the channel is shallow and prone to flooding.

Geographic entities mentioned:
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 43.1256
lon: -93.4247
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 44.75388889
lon: -96.6575
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 46.8675
lon: -122.76666666667
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 28.5219
lon: -81.4103
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 39.0616
lon: -122.8272
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 44.3606
lon: -121.993
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 44.1622
lon: -75.4947
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 46.823611111111
lon: -122.47388888889
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 29.5594
lon: -95.05632
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 45.274722222222
lon: -94.445277777778
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 44.7668323
lon: -97.1762718
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 43.7612743
lon: -97.0121224
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 41.8325
lon: -86.421388888889
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 43.6437495
lon: -124.1824432
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 45.1805262
lon: -121.7089251
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 45.69361111
lon: -97.35944444
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 43.988333333333
lon: -74.920555555556
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 43.900277777778
lon: -95.076944444444
It drains along Scotts Creek into Rodman Slough, which flows into Clear Lake. There is only a slight change in elevation along Scotts Creek between Blue Lakes, Tule Lake and Clear Lake, and the channel is shallow and prone to flooding. Parts of Bachelor Valley may be flooded when Tule Lake backs up and passed through the culverts under highway 20.

Geographic entities mentioned:
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 43.1256
lon: -93.4247
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 44.75388889
lon: -96.6575
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 46.8675
lon: -122.76666666667
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 28.5219
lon: -81.4103
surface_form: blue lakes
instance_of: Lake
countries: United States
coordinates: lat: 39.170398
lon: -123.01134
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 39.0616
lon: -122.8272
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 44.3606
lon: -121.993
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 44.1622
lon: -75.4947
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 46.823611111111
lon: -122.47388888889
surface_form: tule lake
instance_of: Lake
countries: United States
coordinates: lat: 41.909322222222
lon: -121.53304722222
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 29.5594
lon: -95.05632
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 45.274722222222
lon: -94.445277777778
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 44.7668323
lon: -97.1762718
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 43.7612743
lon: -97.0121224
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 41.8325
lon: -86.421388888889
surface_form: tule lake
instance_of: Lake
countries: United States
coordinates: lat: 39.160206
lon: -122.945159
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 43.6437495
lon: -124.1824432
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 45.1805262
lon: -121.7089251
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 45.69361111
lon: -97.35944444
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 43.988333333333
lon: -74.920555555556
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 43.900277777778
lon: -95.076944444444
Parts of Bachelor Valley may be flooded when Tule Lake backs up and passed through the culverts under highway 20. Tule Lake serves to reduce sedimentation in Clear Lake, because the high flows of Scotts Creek spread out in the lake, slow down and drop their sediment. History.

Geographic entities mentioned:
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 43.1256
lon: -93.4247
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 44.75388889
lon: -96.6575
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 46.8675
lon: -122.76666666667
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 28.5219
lon: -81.4103
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 39.0616
lon: -122.8272
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 44.3606
lon: -121.993
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 44.1622
lon: -75.4947
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 46.823611111111
lon: -122.47388888889
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 29.5594
lon: -95.05632
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 45.274722222222
lon: -94.445277777778
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 44.7668323
lon: -97.1762718
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 43.7612743
lon: -97.0121224
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 41.8325
lon: -86.421388888889
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 43.6437495
lon: -124.1824432
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 45.1805262
lon: -121.7089251
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 45.69361111
lon: -97.35944444
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 43.988333333333
lon: -74.920555555556
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 43.900277777778
lon: -95.076944444444
Tule Lake serves to reduce sedimentation in Clear Lake, because the high flows of Scotts Creek spread out in the lake, slow down and drop their sediment. History. The Yima, a group comprising both Northern Pomo and Eastern Pomo, used to live in the area containing Scotts Valley, Blue Lakes, Tule Lake and extended to Clear Lake. They used to camp along the lakeshore during the root-digging season.

Geographic entities mentioned:
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 43.1256
lon: -93.4247
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 44.75388889
lon: -96.6575
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 46.8675
lon: -122.76666666667
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 28.5219
lon: -81.4103
surface_form: blue lakes
instance_of: Lake
countries: United States
coordinates: lat: 39.170398
lon: -123.01134
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 39.0616
lon: -122.8272
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 44.3606
lon: -121.993
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 44.1622
lon: -75.4947
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 46.823611111111
lon: -122.47388888889
surface_form: tule lake
instance_of: Lake
countries: United States
coordinates: lat: 41.909322222222
lon: -121.53304722222
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 29.5594
lon: -95.05632
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 45.274722222222
lon: -94.445277777778
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 44.7668323
lon: -97.1762718
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 43.7612743
lon: -97.0121224
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 41.8325
lon: -86.421388888889
surface_form: tule lake
instance_of: Lake
countries: United States
coordinates: lat: 39.160206
lon: -122.945159
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 43.6437495
lon: -124.1824432
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 45.1805262
lon: -121.7089251
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 45.69361111
lon: -97.35944444
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 43.988333333333
lon: -74.920555555556
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 43.900277777778
lon: -95.076944444444
Tule Lake (Lake County, California). Tule Lake is a seasonal lake in Lake County, California. It is named after the edible bullrushes, or tules, that used to surround the lake. These have been cleared and the lake partly drained to support agriculture, but it still floods every winter. In summer it is used for growing wild rice and grazing cattle.

Geographic entities mentioned:
surface_form: tule lake
instance_of: Lake
countries: United States
coordinates: lat: 41.909322222222
lon: -121.53304722222
surface_form: tule lake
instance_of: Lake
countries: United States
coordinates: lat: 39.160206
lon: -122.945159
There have been proposals to restore the lake to its original wetlands condition. Location. Tule Lake is in Lake County, California at an elevation of. The lake is bordered by Scotts Creek, which defines its south shore, and California State Route 20 to the north. The lake is named after the plentiful tules (&quot;Schoenoplectus acutus&quot;) that used to grow around it. Hydrology.

Geographic entities mentioned:
surface_form: tule lake
instance_of: Lake
countries: United States
coordinates: lat: 41.909322222222
lon: -121.53304722222
surface_form: tule lake
instance_of: Lake
countries: United States
coordinates: lat: 39.160206
lon: -122.945159
It drains along Scotts Creek into Rodman Slough, which flows into Clear Lake. There is only a slight change in elevation along Scotts Creek between Blue Lakes, Tule Lake and Clear Lake, and the channel is shallow and prone to flooding. Parts of Bachelor Valley may be flooded when Tule Lake backs up and passed through the culverts under highway 20.

Geographic entities mentioned:
surface_form: tule lake
instance_of: Lake
countries: United States
coordinates: lat: 41.909322222222
lon: -121.53304722222
surface_form: tule lake
instance_of: Lake
countries: United States
coordinates: lat: 41.909322222222
lon: -121.53304722222
surface_form: tule lake
instance_of: Lake
countries: United States
coordinates: lat: 39.160206
lon: -122.945159
surface_form: tule lake
instance_of: Lake
countries: United States
coordinates: lat: 39.160206
lon: -122.945159
They used to camp along the lakeshore during the root-digging season. Tule Lake has deep alluvial soils and silty clay loam, suitable for field crops. In 1891 European settlers began growing and canning string beans near Tule Lake. Henry Wambold, who built the Laurel Dell Hotel, built a string bean cannery in 1891.

Geographic entities mentioned:
surface_form: tule lake
instance_of: Lake
countries: United States
coordinates: lat: 41.909322222222
lon: -121.53304722222
surface_form: tule lake
instance_of: Lake
countries: United States
coordinates: lat: 39.160206
lon: -122.945159