Sarmila/GeoWiki-Features huggingface dataset:
While driving a long adit from an elevation of into the Cape Mountain, close to the peak, for prospecting for minerals, biotite granite formation of the hill revealed cassiterite-bearing quartz of the Late Cretaceous period. The evolution of the Cape Mountain granite has been &quot;determined to be 78.8 +/- 2.9 my old by the K/Ar method&quot;. Mineral prospecting.

Geographic entities mentioned:
surface_form: cape mountain
instance_of: Mountain
countries: United States
coordinates: lat: 65.576389
lon: -168.0075
&quot;City of Bangor&quot; was a freighter that had a 30-year career on the Great Lakes. Originally designed to carry ore, the ship was converted into an automobile carrier in 1925. She was trapped in ice on Lake Superior November 30, 1926, and after multiple salvage attempts, &quot;Bangor&quot; was declared a total loss. Shipwreck. &quot;City of Bangor&quot; was captained by William J. Mackin.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
The nearest community is Sesekinika, to the east. The lake is about long and wide. The primary inflow is Lillord Creek arriving at the northwest from Lillord Lake. There is a secondary inflow at the southeast. The primary outflow, at the northeast, is Lillord Creek, which flows southeast on the way to its mouth at the Blanche River.

Geographic entities mentioned:
surface_form: Lillord Lake
instance_of: Lake
countries: Canada
coordinates: lat: 48.208888888888886
lon: -80.30416666666666
The lake is about long and wide. The primary inflow is Lillord Creek arriving at the northwest from Lillord Lake. There is a secondary inflow at the southeast. The primary outflow, at the northeast, is Lillord Creek, which flows southeast on the way to its mouth at the Blanche River. The Blanche River flows via Lake Timiskaming and the Ottawa River to the Saint Lawrence River.

Geographic entities mentioned:
surface_form: Lake Timiskaming
instance_of: Lake
countries: Canada
coordinates: lat: 47.333333333333
lon: -79.5
surface_form: blanche river
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.83969
lon: -71.69266
surface_form: blanche river
instance_of: Watercourse
countries: Canada
coordinates: lat: 47.93055556
lon: -74.10138889
Berube Lake. Berube Lake is a lake in geographic Lee Township in the Unorganized West Part of Timiskaming District, in northeastern Ontario, Canada. The lake is in the Saint Lawrence River drainage basin and is on Lillord Creek. The nearest community is Sesekinika, to the east. The lake is about long and wide. The primary inflow is Lillord Creek arriving at the northwest from Lillord Lake.

Geographic entities mentioned:
surface_form: berube lake
instance_of: Lake
countries: Canada
coordinates: lat: 48.20472222222222
lon: -80.3
The lake is about long and wide. The primary inflow is Lillord Creek arriving at the northwest from Lillord Lake. There is a secondary inflow at the southeast. The primary outflow, at the northeast, is Lillord Creek, which flows southeast on the way to its mouth at the Blanche River. The Blanche River flows via Lake Timiskaming and the Ottawa River to the Saint Lawrence River.

Geographic entities mentioned:
surface_form: blanche river
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.83969
lon: -71.69266
surface_form: blanche river
instance_of: Watercourse
countries: Canada
coordinates: lat: 47.93055556
lon: -74.10138889
Mount Karadağ. Karadağ (literally: &quot;Black mountain&quot;) is an extinct volcano in Karaman Province, Turkey. The mountain, which was heavily inhabited in the Hittite and Byzantine periods, is now used mostly for telecommunications, but many historical structures are still visible. Geography. The Karadağ volcano rises between the Çumra lowlands and the Hotamış marsh.

Geographic entities mentioned:
surface_form: karadağ
instance_of: Mountain
countries: Turkey
coordinates: lat: 37.3994
lon: 33.14711
surface_form: mount karadağ
instance_of: Mountain
countries: Turkey
coordinates: lat: 37.3994
lon: 33.14711
Mount Karadağ. Karadağ (literally: &quot;Black mountain&quot;) is an extinct volcano in Karaman Province, Turkey. The mountain, which was heavily inhabited in the Hittite and Byzantine periods, is now used mostly for telecommunications, but many historical structures are still visible. Geography. The Karadağ volcano rises between the Çumra lowlands and the Hotamış marsh.

Geographic entities mentioned:
surface_form: karadağ
instance_of: Mountain
countries: Turkey
coordinates: lat: 37.3994
lon: 33.14711
Flora and fauna. The region is home to around 250 wild horses and many feral sheep. The mountain Karadağ is located near the Mediterranean Sea, which means its climate is a mix of Mediterranean and continental climate. Due to this, the area is mostly covered by maquis. However, there are also some endemic plants, including the &quot;Astragalus vestitus&quot;. Geologic history.

Geographic entities mentioned:
surface_form: karadağ
instance_of: Mountain
countries: Turkey
coordinates: lat: 37.3994
lon: 33.14711
During the expedition, Father Crespí observed a location along the river that would be good for a settlement or mission. However, in 1771, Father Serra instead commissioned two missionaries to establish the Mission San Gabriel Arcángel-San Gabriel Mission near the present day Whittier Narrows section of the San Gabriel River.

Geographic entities mentioned:
surface_form: Whittier Narrows
instance_of: Landform
countries: United States
coordinates: lat: 34.0292
lon: -118.049
Lieutenant-Colonel Frémont and Governor of Alta California Andrés Pico signed the Treaty of Cahuenga, an informal agreement to cease fighting in California at the Campo de Cahuenga in the San Fernando Valley in January 1847.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
Somma volcano. A somma volcano, also known as a sommian, is a volcanic caldera that has been partially filled by a new central cone. The type is named after Mount Somma (&quot;Summit&quot;), a stratovolcano in southern Italy with a summit caldera in which the upper cone of Mount Vesuvius has grown.

Geographic entities mentioned:
surface_form: Mount Vesuvius
instance_of: Mountain
countries: Italy
coordinates: lat: 40.821388888889
lon: 14.425555555556
Jerichow Monastery. The Jerichow Monastery () is a former Premonstratensian monastery located in the northern outskirts of Jerichow, near the shores of the Elbe River, in the state of Saxony-Anhalt of Germany. Founded by the Premonstratensians, it was &quot;not&quot; a monastery but the Collegiate Church of St. Mary and St. Nicholas.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
Aatunselkä. Aatunselkä is a lake in the municipality of Äänekoski in the Central Finland Province in Finland. Details. The lake is 91.7 m above sea level. The area is 1.05 square km and the Coast is 10.41 km long. The lake is part of the Kymi (river)'s main catchment area. It is located about 33 km north of Jyväskylä and about 270 km north of Helsinki.

Geographic entities mentioned:
surface_form: aatunselkä
instance_of: Lake
countries: Finland
coordinates: lat: 62.5452
lon: 25.8185
Sude (river). The Sude () is a river in Mecklenburg-Vorpommern and Lower Saxony, Germany. Its source is near Renzow (a district of Schildetal) in western Mecklenburg. It flows through the lake Dümmer See, and continues past Hagenow and Lübtheen. It flows into the Elbe in Boizenburg.

Geographic entities mentioned:
surface_form: Dümmer See
instance_of: Lake
countries: Germany
coordinates: lat: 53.581388888889
lon: 11.202777777778
Sude (river). The Sude () is a river in Mecklenburg-Vorpommern and Lower Saxony, Germany. Its source is near Renzow (a district of Schildetal) in western Mecklenburg. It flows through the lake Dümmer See, and continues past Hagenow and Lübtheen. It flows into the Elbe in Boizenburg.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
Lower Erebus Hut. The Lower Erebus Hut (LEH) is a permanent field facility located on Mount Erebus on Ross Island, Antarctica. The hut served as the seasonal base of the Mount Erebus Volcano Observatory (MEVO), run by New Mexico Institute of Mining and Technology (NMT). The installation comprises two huts, one kitchen and recreation building and one working and storage building.

Geographic entities mentioned:
surface_form: Mount Erebus
instance_of: Mountain
coordinates: lat: -77.533333333333
lon: 167.28333333333
Long Island Pond (Plymouth, Massachusetts). Long Island Pond, also known as Little Island Pond, is a pond in Plymouth, Massachusetts. The pond is located in the eastern portion of &quot;The Pinehills&quot; development north of Great Island Pond and south of Beaver Dam Pond.

Geographic entities mentioned:
surface_form: Great Island Pond
instance_of: Lake
countries: United States
coordinates: lat: 41.884722222222
lon: -70.573055555556
surface_form: island pond
instance_of: Lake
countries: United States
coordinates: lat: 43.0667
lon: -72.0842
Long Island Pond (Plymouth, Massachusetts). Long Island Pond, also known as Little Island Pond, is a pond in Plymouth, Massachusetts. The pond is located in the eastern portion of &quot;The Pinehills&quot; development north of Great Island Pond and south of Beaver Dam Pond.

Geographic entities mentioned:
surface_form: long island pond
instance_of: Lake
countries: United States
coordinates: lat: 41.8944
lon: -70.5764
surface_form: island pond
instance_of: Lake
countries: United States
coordinates: lat: 43.0667
lon: -72.0842
Long Island Pond (Plymouth, Massachusetts). Long Island Pond, also known as Little Island Pond, is a pond in Plymouth, Massachusetts. The pond is located in the eastern portion of &quot;The Pinehills&quot; development north of Great Island Pond and south of Beaver Dam Pond.

Geographic entities mentioned:
surface_form: long island pond
instance_of: Lake
countries: United States
coordinates: lat: 41.8944
lon: -70.5764
surface_form: island pond
instance_of: Lake
countries: United States
coordinates: lat: 43.0667
lon: -72.0842
surface_form: island pond
instance_of: Lake
countries: United States
coordinates: lat: 43.0667
lon: -72.0842
Monte San Giorgio. Monte San Giorgio is a Swiss mountain and UNESCO World Heritage Site near the border between Switzerland and Italy. It is part of the Lugano Prealps, overlooking Lake Lugano in the Swiss Canton of Ticino. Monte San Giorgio is a wooded mountain, rising to 1,097 m (3,600 feet) above sea level.

Geographic entities mentioned:
surface_form: Lake Lugano
instance_of: Lake
countries: Switzerland
Italy
coordinates: lat: 46
lon: 9
This was in recognition of its cultural, biological, and especially paleontological significance. The site is renowned for its fossil content, one of the best known records of marine life in the Middle Triassic period. The Italian region west of Poncione d'Arzo (Porto Ceresio) was added as an extension to the World Heritage Site in 2010. History and cultural heritage.

Geographic entities mentioned:
surface_form: Poncione d'Arzo
instance_of: Mountain
countries: Switzerland
Italy
coordinates: lat: 45.89181
lon: 8.92715
Its Jurassic sediments are now eroded away to reveal older Triassic and Permian rocks. Conversely, Monte Generoso, immediately to the east of Monte San Giorgio, is composed mostly of Jurassic basinal sediments. Outcrops of Jurassic sediments are also seen close to the Po Plain, at the south edge of Monte San Giorgio (in a broad sense).

Geographic entities mentioned:
surface_form: Monte Generoso
instance_of: Mountain
countries: Switzerland
Italy
coordinates: lat: 45.929444444444
lon: 9.0191666666667
Conversely, Monte Generoso, immediately to the east of Monte San Giorgio, is composed mostly of Jurassic basinal sediments. Outcrops of Jurassic sediments are also seen close to the Po Plain, at the south edge of Monte San Giorgio (in a broad sense). The productive &quot;marble&quot; quarries found south of Monte San Giorgio actually mined non-metamorphosed limestone, rather than true marble.

Geographic entities mentioned:
surface_form: sense
instance_of: Watercourse
countries: Switzerland
coordinates: lat: 46.906
lon: 7.23389
surface_form: monte san giorgio
instance_of: Mountain
countries: Switzerland
coordinates: lat: 45.916666666667
lon: 8.95
surface_form: monte san giorgio
instance_of: Mountain
countries: Switzerland
coordinates: lat: 45.916666666667
lon: 8.95
Minerals such as barite, fluorite, and galena were also prospected on the mountain during the 20th century. Italian paleontologist Giulio Curioni first mentioned that fossils were present on the mountain in 1847. The first paper focusing on Monte San Giorgio fossils in particular was published by Emilio Cornalia in 1854.

Geographic entities mentioned:
surface_form: first
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.50486111
lon: 7.64305556
surface_form: first
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.6608
lon: 8.05469
Italian paleontologist Giulio Curioni first mentioned that fossils were present on the mountain in 1847. The first paper focusing on Monte San Giorgio fossils in particular was published by Emilio Cornalia in 1854. Small excavations by Milanese paleontological societies in 1863 and 1878 provided more specific context on the paleontology of Monte San Giorgio.

Geographic entities mentioned:
surface_form: first
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.50486111
lon: 7.64305556
surface_form: monte san giorgio
instance_of: Mountain
countries: Switzerland
coordinates: lat: 45.916666666667
lon: 8.95
surface_form: first
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.6608
lon: 8.05469
Local museums in Besano, Meride, and Induno Olona also play a role in promotion of the site and its fossils. The (Museum of fossils from Monte San Giorgio) in Meride was first opened 1973, receiving a 2012 redesign and expansion courtesy of Ticinese architect Mario Botta. Geology. The geological layers of Monte San Giorgio span more than 100 million years, from the Permian to Jurassic periods.

Geographic entities mentioned:
surface_form: first
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.50486111
lon: 7.64305556
surface_form: monte san giorgio
instance_of: Mountain
countries: Switzerland
coordinates: lat: 45.916666666667
lon: 8.95
surface_form: first
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.6608
lon: 8.05469
These following Triassic sediments are siliciclastic and terrestrial in origin, mainly sandstone and conglomerate eroded from the underlying volcanic material. &quot;Servino&quot; is the name given to older sediments from the Early Triassic (about 252-247 Ma). Slightly younger sediments from the late Anisian (the first stage of the Middle Triassic, 247-242 Ma) are called the Bellano Formation.

Geographic entities mentioned:
surface_form: first
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.50486111
lon: 7.64305556
surface_form: first
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.6608
lon: 8.05469
As the Anisian stage continued, the coastal sandstone of the Bellano Formation was replaced with calcareous marine deposits. These were the first of many massive carbonate platforms building up on a branch of the Tethys Sea which was expanding westwards.

Geographic entities mentioned:
surface_form: first
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.50486111
lon: 7.64305556
surface_form: first
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.6608
lon: 8.05469
This formation has been called the Besano Formation (in Italy) or the Grenzbitumenzone (in Switzerland). It represents the first of several sections on the mountain enriched with well-preserved fossils. The Grenzbitumenzone, especially its shale layers, is enriched with organic material derived from cyanobacteria.

Geographic entities mentioned:
surface_form: first
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.50486111
lon: 7.64305556
surface_form: first
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.6608
lon: 8.05469
In the succeeding Norian stage (around 227 to ~208 Ma), carbonate platforms and rising sea levels were renewed with vigor, depositing a massive expanse of carbonate known as the Dolomia Principale or Hauptdolomit. The Dolomia Principale is a brittle, crystalline rock mass which was fractured by normal faults not long after it was first formed.

Geographic entities mentioned:
surface_form: first
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.50486111
lon: 7.64305556
surface_form: first
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.6608
lon: 8.05469
These were the first of many massive carbonate platforms building up on a branch of the Tethys Sea which was expanding westwards. The shallow carbonate platform of Monte San Giorgio and surrounding areas is known as the Salvatore platform, which is now preserved as the San Salvatore Dolomite.

Geographic entities mentioned:
surface_form: san salvatore
instance_of: Mountain
countries: Switzerland
coordinates: lat: 45.976666666667
lon: 8.9480555555556
surface_form: monte san giorgio
instance_of: Mountain
countries: Switzerland
coordinates: lat: 45.916666666667
lon: 8.95
It reconstructs a warm, tropical environment, with the most common fossils belonging to algae and shelled invertebrates. Only the lower portion of the San Salvatore Dolomite is preserved on Monte San Giorgio, corresponding to a particularly shallow and saline period in the history of the platform.

Geographic entities mentioned:
surface_form: san salvatore
instance_of: Mountain
countries: Switzerland
coordinates: lat: 45.976666666667
lon: 8.9480555555556
surface_form: monte san giorgio
instance_of: Mountain
countries: Switzerland
coordinates: lat: 45.916666666667
lon: 8.95
Monte San Giorgio. Monte San Giorgio is a Swiss mountain and UNESCO World Heritage Site near the border between Switzerland and Italy. It is part of the Lugano Prealps, overlooking Lake Lugano in the Swiss Canton of Ticino. Monte San Giorgio is a wooded mountain, rising to 1,097 m (3,600 feet) above sea level.

Geographic entities mentioned:
surface_form: monte san giorgio
instance_of: Mountain
countries: Switzerland
coordinates: lat: 45.916666666667
lon: 8.95
It is part of the Lugano Prealps, overlooking Lake Lugano in the Swiss Canton of Ticino. Monte San Giorgio is a wooded mountain, rising to 1,097 m (3,600 feet) above sea level. It has a roughly pyramidal shape, with a steep north edge sloping towards Lake Lugano and a more shallow South Slope extending towards the Po Plain.

Geographic entities mentioned:
surface_form: monte san giorgio
instance_of: Mountain
countries: Switzerland
coordinates: lat: 45.916666666667
lon: 8.95
History and cultural heritage. Humans have inhabited Monte San Giorgio at least since the area's equivalent of the Neolithic Period, around 6,000 years ago. The south side of the mountain is home to Tremona-Castello Archaeological Park, a fortress and settlement which was continuously inhabited by artisans from the Neolithic up until the 14th century.

Geographic entities mentioned:
surface_form: monte san giorgio
instance_of: Mountain
countries: Switzerland
coordinates: lat: 45.916666666667
lon: 8.95
The first paper focusing on Monte San Giorgio fossils in particular was published by Emilio Cornalia in 1854. Small excavations by Milanese paleontological societies in 1863 and 1878 provided more specific context on the paleontology of Monte San Giorgio. Shale extraction brought the fossil deposits to the attention of University of Zurich paleontologist Bernhard Peyer in 1919.

Geographic entities mentioned:
surface_form: monte san giorgio
instance_of: Mountain
countries: Switzerland
coordinates: lat: 45.916666666667
lon: 8.95
World War II paused both Saurol production and fossil collection. The Museo Civico di Storia Naturale di Milano (Milan Civic Museum of Natural History, MSNM) was bombed in 1943, destroying its collection of Monte San Giorgio specimens. Fossil excavations resumed in 1950 under the helm of Emil Kuhn-Schnyder, Peyer's successor and former student.

Geographic entities mentioned:
surface_form: monte san giorgio
instance_of: Mountain
countries: Switzerland
coordinates: lat: 45.916666666667
lon: 8.95
Fossil excavations resumed in 1950 under the helm of Emil Kuhn-Schnyder, Peyer's successor and former student. Kuhn-Schnyder established the Palaeontological Institute and Museum of the University of Zurich (PIMUZ) in 1956, which now hosts over 15,000 specimens of Monte San Giorgio fossils.

Geographic entities mentioned:
surface_form: monte san giorgio
instance_of: Mountain
countries: Switzerland
coordinates: lat: 45.916666666667
lon: 8.95
Over 21,000 fossil specimens have been collected in total by 2010. UNESCO listing. In 2003, the Monte San Giorgio was listed as a UNESCO World Heritage Site, with 849 ha (hectares) of protected land from the Swiss communes of Meride, Brusino Arsizio, and Riva San Vitale. This protected area was surrounded by a 1389 ha buffer zone overlapping six additional communes.

Geographic entities mentioned:
surface_form: monte san giorgio
instance_of: Mountain
countries: Switzerland
coordinates: lat: 45.916666666667
lon: 8.95
This protected area was surrounded by a 1389 ha buffer zone overlapping six additional communes. The nomination of Monte San Giorgio was inspired by its exceptional paleontological value, with multiple fossiliferous levels preserving among the best records of Middle Triassic life in the world.

Geographic entities mentioned:
surface_form: monte san giorgio
instance_of: Mountain
countries: Switzerland
coordinates: lat: 45.916666666667
lon: 8.95
The nomination of Monte San Giorgio was inspired by its exceptional paleontological value, with multiple fossiliferous levels preserving among the best records of Middle Triassic life in the world. Monte San Giorgio also presents a link between local geology and culture, as well as unique ecological heritage relative to the rest of Switzerland.

Geographic entities mentioned:
surface_form: monte san giorgio
instance_of: Mountain
countries: Switzerland
coordinates: lat: 45.916666666667
lon: 8.95
The site is not in any particular danger from overutilization or degradation, so management is mainly related to closely-regulated fossil excavations, promotion, and maintenance of low-impact tourism facilities. Monte San Giorgio fossils are collected, curated, and displayed by a small number of museums, primarily the PIMUZ, MSNM, and MCSN.

Geographic entities mentioned:
surface_form: monte san giorgio
instance_of: Mountain
countries: Switzerland
coordinates: lat: 45.916666666667
lon: 8.95
Geology. The geological layers of Monte San Giorgio span more than 100 million years, from the Permian to Jurassic periods. The rocks forming the mountain dip southwards, with older rocks exposed as one travels north and younger rocks exposed as one travels south. The oldest rocks are Permian volcanic basement material on the mountain's steep north slope.

Geographic entities mentioned:
surface_form: monte san giorgio
instance_of: Mountain
countries: Switzerland
coordinates: lat: 45.916666666667
lon: 8.95
Permian volcanics and Triassic transgression. The stratigraphically lowest rocks exposed on Monte San Giorgio are Lower Permian in age, around 290-280 Ma (million years old). They are remnants of early rifting and volcanic activity in the aftermath of the Variscan orogeny.

Geographic entities mentioned:
surface_form: monte san giorgio
instance_of: Mountain
countries: Switzerland
coordinates: lat: 45.916666666667
lon: 8.95
Grenzbitumenzone / Besano Formation. Near the end of the Anisian, the southern edge of the Salvatore platform deepens abruptly, giving way to a more sterile basin developed between carbonate platforms. The basin is now preserved as a relatively narrow band of dark dolomite and shale, running east to west along the edge of Monte San Giorgio.

Geographic entities mentioned:
surface_form: monte san giorgio
instance_of: Mountain
countries: Switzerland
coordinates: lat: 45.916666666667
lon: 8.95
These basin sediments are preserved as the Moltrasio Limestone, a thick sheet of micrite (fine-grained limestone) with abundant cherty and marly beds created by turbidites (mudslides). Jurassic sediments are preserved to the east, south, and west of Monte San Giorgio; the position of the modern mountain would have been an island or shallow environment during the Jurassic.

Geographic entities mentioned:
surface_form: monte san giorgio
instance_of: Mountain
countries: Switzerland
coordinates: lat: 45.916666666667
lon: 8.95
The driest and most alkaline soils of Monte San Giorgio are home to the Ticino dry meadows, a unique biome with over 100 plant and species, 38 of which are rare or endangered within Switzerland.

Geographic entities mentioned:
surface_form: monte san giorgio
instance_of: Mountain
countries: Switzerland
coordinates: lat: 45.916666666667
lon: 8.95
&quot;Carex humilis&quot; (dwarf sedge) and &quot;Molinia caerulea arundinacea&quot; (tall moor grass) are the most common grasses, while Monte San Giorgio supports the few Swiss populations of wildflowers such as &quot;Adenophora liliifolia&quot;, &quot;Gladiolus imbricatus&quot;, &quot;Iris graminea&quot;, &quot;Lotus herbaceus&quot;, and &quot;Danthonia alpina&quot;.

Geographic entities mentioned:
surface_form: monte san giorgio
instance_of: Mountain
countries: Switzerland
coordinates: lat: 45.916666666667
lon: 8.95
Antikyra is situated on the () on the north coast of the Gulf of Corinth. It lies southwest of Paralia Distomou (also formerly known as &quot;Aspra Spitia&quot;) and southeast of Desfina. It is separated from Delphi by Mount Cirphis and from the Crissaean Gulf by the Opus peninsula (). The municipal unit also contains the villages of Agia Sotira and Agios Isidoros.

Geographic entities mentioned:
surface_form: Mount Cirphis
instance_of: Mountain
countries: Greece
coordinates: lat: 38.462
lon: 22.499
Together with Santok and Drezdenko, it remained the seat of a (Greater) Polish castellany on the Pomeranian border in the 12th and 13th centuries. With adjacent Lubusz Land in the south, the town became a part of the &quot;Neumark&quot; acquisitions of the Ascanian margraves John I and of Otto III of Brandenburg in 1248/52.

Geographic entities mentioned:
surface_form: Lubusz Land
instance_of: Plateau
countries: Germany
Poland
Kingdom of Poland
Lands of the Bohemian Crown
Ladhar Bheinn. Ladhar Bheinn is the highest mountain in the Knoydart region of the Highlands of Scotland. It is the most westerly Munro on the Scottish mainland. The mountain may be climbed from Barrisdale to the northeast or Inverie to the south.

Geographic entities mentioned:
surface_form: ladhar bheinn
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.075263
lon: -5.591745
Snake River Land Company Residence and Office. The Snake River Land Company Residence and Office are structures associated with John D. Rockefeller Jr.'s acquisition of land in Jackson Hole, Wyoming, United States.

Geographic entities mentioned:
surface_form: Jackson Hole
instance_of: Valley
countries: United States
coordinates: lat: 43.516666666667
lon: -110.83333333333
Gilpin Peak. Gilpin Peak is a high mountain summit in the Sneffels Range of the Rocky Mountains of North America. The thirteener is located in the Mount Sneffels Wilderness of Uncompahgre National Forest, north-northeast (bearing 23°) of the Town of Telluride, Colorado, United States, on the drainage divide between Ouray County and San Miguel County.

Geographic entities mentioned:
surface_form: high mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.0887
lon: -74.2351
surface_form: sneffels
instance_of: Mountain
countries: United States
coordinates: lat: 38.003888888889
lon: -107.79222222222
surface_form: gilpin peak
instance_of: Mountain
countries: United States
coordinates: lat: 37.9867
lon: -107.793
Gilpin Peak. Gilpin Peak is a high mountain summit in the Sneffels Range of the Rocky Mountains of North America. The thirteener is located in the Mount Sneffels Wilderness of Uncompahgre National Forest, north-northeast (bearing 23°) of the Town of Telluride, Colorado, United States, on the drainage divide between Ouray County and San Miguel County.

Geographic entities mentioned:
surface_form: sneffels
instance_of: Mountain
countries: United States
coordinates: lat: 38.003888888889
lon: -107.79222222222
surface_form: mount sneffels
instance_of: Mountain
countries: United States
coordinates: lat: 38.003888888889
lon: -107.79222222222
Gilpin Peak. Gilpin Peak is a high mountain summit in the Sneffels Range of the Rocky Mountains of North America. The thirteener is located in the Mount Sneffels Wilderness of Uncompahgre National Forest, north-northeast (bearing 23°) of the Town of Telluride, Colorado, United States, on the drainage divide between Ouray County and San Miguel County.

Geographic entities mentioned:
surface_form: gilpin peak
instance_of: Mountain
countries: United States
coordinates: lat: 37.9867
lon: -107.793
The thirteener is located in the Mount Sneffels Wilderness of Uncompahgre National Forest, north-northeast (bearing 23°) of the Town of Telluride, Colorado, United States, on the drainage divide between Ouray County and San Miguel County. Gilpin Peak was named in honor of William Gilpin, the first Governor of the Territory of Colorado. Climate.

Geographic entities mentioned:
surface_form: gilpin peak
instance_of: Mountain
countries: United States
coordinates: lat: 37.9867
lon: -107.793
Climate. According to the Köppen climate classification system, Gilpin Peak is located in an alpine subarctic climate zone with long, cold, snowy winters, and cool to warm summers. Due to its altitude, it receives precipitation all year, as snow in winter, and as thunderstorms in summer, with a dry period in late spring.

Geographic entities mentioned:
surface_form: gilpin peak
instance_of: Mountain
countries: United States
coordinates: lat: 37.9867
lon: -107.793
In 1964, the Cuban government stopped the flow. The base had about of water in storage, and strict water conservation was put into effect immediately. The U.S. first imported water from Jamaica by barge, then relocated a desalination plant from San Diego (Point Loma). When the Cuban government accused the United States of &quot;stealing water&quot;, base commander John D.

Geographic entities mentioned:
surface_form: Point Loma
instance_of: Landform
countries: United States
coordinates: lat: 32.67
lon: -117.24194444
Mount Overill. Mount Overill is a volcanic peak in southwestern British Columbia, Canada, located east of Rivers Inlet and northwest of Mount Somolenko.

Geographic entities mentioned:
surface_form: Mount Somolenko
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4694
lon: -126.103
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: mount overill
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4769
lon: -126.131
Mount Overill. Mount Overill is a volcanic peak in southwestern British Columbia, Canada, located east of Rivers Inlet and northwest of Mount Somolenko.

Geographic entities mentioned:
surface_form: mount overill
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4769
lon: -126.131
Farm to Market Roads in Texas are owned and maintained by the Texas Department of Transportation (TxDOT). FM 800. Farm to Market Road 800 (FM 800) is located in Cameron County in the Lower Rio Grande Valley. FM 800 begins at an intersection with FM 2520 southwest of San Benito. The highway travels in a northwest direction and intersects FM 509 and FM 1479 in Rangerville.

Geographic entities mentioned:
surface_form: Lower Rio Grande Valley
instance_of: Valley
countries: United States
Mexico
coordinates: lat: 26.22
lon: -98.12
The Doberdò area has a crucial strategic position. A relatively wide and flat canyon runs right through the middle of the municipality from north to south, connecting the Vipava Valley to the Adriatic Sea. The canyon is called simply &quot;Dol&quot; (Slovene for vale).

Geographic entities mentioned:
surface_form: Vipava Valley
instance_of: Valley
countries: Slovenia
coordinates: lat: 45.876147222222
lon: 13.907319444444
According to the U.S. Census Bureau, the Heathcote CDP has an area of, including of water (0.16%). The community lies on a slope that drains south toward Heathcote Brook, a west-flowing tributary of the Millstone River, part of the Raritan River watershed. 2010 census. The 2010 United States census counted 5,821 people, 2,326 households, and 1,558 families in the CDP. The population density was.

Geographic entities mentioned:
surface_form: Heathcote Brook
instance_of: Landform
countries: United States
coordinates: lat: 40.37361111
lon: -74.62
New York State Route 96 is an east–west highway passing through the village. The New York State Thruway passes north of the village. Flint Creek flows through the village to the Canandaigua Outlet. Phelps is in the Finger Lakes District and is north of Seneca Lake. Demographics. As of the census of 2000, there were 1,969 people, 791 households, and 521 families residing in the village.

Geographic entities mentioned:
surface_form: Finger Lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 42.666666666667
lon: -76.833333333333
First College of Sant'Anselmo. By the early 15th century, the number of Benedictine monasteries connected with the Archabbey of Monte Cassino varied in membership from very small to very large. As such, a &quot;Cassinese Benedictine Congregation&quot; was formed in 1408 to affiliate those monasteries connected with the archabbey as a means of support and cooperation.

Geographic entities mentioned:
surface_form: Archabbey of Monte Cassino
instance_of: Mountain
countries: Italy
coordinates: lat: 41.49
lon: 13.813888888889
Further challenging the students was the sudden death in 1942 of Fr. Anselm Stolz of Gerleve Abbey who had served as an internationally famous monk and professor. Finally, in October 1943, the monastic community of the Archabbey of Monte Cassino, along with their archives and artwork, were transferred to Sant'Anselmo before the final destruction of that monastery. Post war years.

Geographic entities mentioned:
surface_form: Archabbey of Monte Cassino
instance_of: Mountain
countries: Italy
coordinates: lat: 41.49
lon: 13.813888888889
Maumee Bay State Park. Maumee Bay State Park is a public recreation area located on the shores of Lake Erie, five miles east of Toledo, in Jerusalem Township, Lucas County, Ohio, United States. Major features of the state park include a lodge and conference center, cottages, camping facilities, golf course, nature center, and two-mile-long interpretive boardwalk.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
The locomotive was not classified, but named &quot;Portuguese&quot; and referred to by name. Narrow gauge. In 1903, the CGR placed six Type B locomotives with eight-wheeled bogie tenders in service on the Avontuur narrow gauge line in the Langkloof. They were built by W. G. Bagnall and had bar frames, copper fireboxes and Stephenson valve gear.

Geographic entities mentioned:
surface_form: Langkloof
instance_of: Valley
countries: South Africa
coordinates: lat: -33.825
lon: 23.857777777778
Balasagan. Balāsagān (an Iranian toponym meaning &quot;country of Balas&quot;; Armenian: &quot;Bałasakan&quot;, the inhabitants known as &quot;Bałasičkʻ,&quot; Arabic: &quot;Balāsajān&quot;/&quot;Balāšajān&quot;), also known as Bazgan, was a region located in the area of the Kura and Aras rivers, adjacent to the Caspian Sea. To the south, it bordered Atropatene/Adurbadagan and Gilan.

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
Furthermore, one of the accords of the peace treaty concluded between the Arab commander Hudhayfah ibn al-Yaman and the &quot;marzban&quot; (margrave) of Adurbadagan was that the Arabs were to protect the locals against the Kurds of Balasagan and the Sabalan mountains. The name of Balasagan rarely appears in classical Arabic chronicles, being replaced with Mughan.

Geographic entities mentioned:
surface_form: Sabalan
instance_of: Mountain
countries: Iran
coordinates: lat: 38.266944444444
lon: 47.836944444444
British planning. Loudoun's plan for the 1757 campaign was submitted to the government in London in September 1756, focused on a single expedition aimed at the heart of New France in the city of Quebec. It called for a purely defensive posture along the frontier with New France, including the contested corridor of the Hudson River and Lake Champlain between Albany, New York and Montreal.

Geographic entities mentioned:
surface_form: Lake Champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
Little Bonnet Lake. Little Bonnet Lake, in Highlands County, Florida, is about west of Lake Letta and about twice as far south of Lake Lotela. This lake is bounded on the southwest by a rail line and on the southeast and part of the north side by citrus groves. Woods are on the east, part of the west and part of the north. A golf course borders Little Bonnet Lake on the northwest.

Geographic entities mentioned:
surface_form: Lake Letta
instance_of: Lake
countries: United States
coordinates: lat: 27.5611
lon: -81.4626
surface_form: Lake Lotela
instance_of: Lake
countries: United States
coordinates: lat: 27.57694
lon: -81.48245
surface_form: little bonnet lake
instance_of: Lake
countries: United States
coordinates: lat: 27.562
lon: -81.4759
surface_form: bonnet lake
instance_of: Lake
countries: United States
coordinates: lat: 27.5436
lon: -81.442
Little Bonnet Lake. Little Bonnet Lake, in Highlands County, Florida, is about west of Lake Letta and about twice as far south of Lake Lotela. This lake is bounded on the southwest by a rail line and on the southeast and part of the north side by citrus groves. Woods are on the east, part of the west and part of the north. A golf course borders Little Bonnet Lake on the northwest.

Geographic entities mentioned:
surface_form: little bonnet lake
instance_of: Lake
countries: United States
coordinates: lat: 27.562
lon: -81.4759
surface_form: bonnet lake
instance_of: Lake
countries: United States
coordinates: lat: 27.5436
lon: -81.442
This lake is bounded on the southwest by a rail line and on the southeast and part of the north side by citrus groves. Woods are on the east, part of the west and part of the north. A golf course borders Little Bonnet Lake on the northwest. On the lake's northeast shore is a public boat ramp, that is reached by going through the area's golf course.

Geographic entities mentioned:
surface_form: little bonnet lake
instance_of: Lake
countries: United States
coordinates: lat: 27.562
lon: -81.4759
surface_form: bonnet lake
instance_of: Lake
countries: United States
coordinates: lat: 27.5436
lon: -81.442
A golf course borders Little Bonnet Lake on the northwest. On the lake's northeast shore is a public boat ramp, that is reached by going through the area's golf course. A canal allows boats to travel east to Lake Letta and by a series of canals a number of area lakes may be accessed from Little Bonnet Lake. There are no public swimming beaches, but fishing is allowed.

Geographic entities mentioned:
surface_form: little bonnet lake
instance_of: Lake
countries: United States
coordinates: lat: 27.562
lon: -81.4759
surface_form: bonnet lake
instance_of: Lake
countries: United States
coordinates: lat: 27.5436
lon: -81.442
surface_form: lake letta
instance_of: Lake
countries: United States
coordinates: lat: 27.5611
lon: -81.4626
Ecology. &quot;Ficus vasta&quot; grows in or near the Horn of Africa. It is primarily endemic to Ethiopia and Yemen, but can also be found in the Sudan, Somalia and Saudi Arabia, and into Uganda and Tanzania in the African Great Lakes region. The tree grows along rivers forming stands or thickets. Additionally, it is found in dry savannah and grows at elevations between.

Geographic entities mentioned:
surface_form: African Great Lakes
instance_of: Group of lakes
countries: Burundi
Zambia
Kenya
Democratic Republic of the Congo
Malawi
Mozambique
Rwanda
Tanzania
Uganda
Ethiopia
coordinates: lat: -8
lon: 35
MacMahon. Overview. Moving through the turn of the century, Musical Association toured the Mohawk Valley, Hudson Valley and western New England. The Glee Club was entered into many Intercollegiate Glee Club contests and was a several-time state and regional champion. At the 1931 IMC festival at Carnegie Hall, the Union Men's Glee Club under the direction of Elmer A.

Geographic entities mentioned:
surface_form: Mohawk Valley
instance_of: Valley
countries: United States
surface_form: Hudson Valley
instance_of: Valley
countries: United States
coordinates: lat: 41.9209
lon: -73.9613
Puente Rayitos de Sol. Rayitos de Sol Bridge () is a pedestrian bridge in the historic centre of Lima, Peru. It crosses the Rímac river, connecting the Vía de Evitamiento with the Alameda Chabuca Granda. History. The bridge was inaugurated on November 7, 2006, and cost . two and a half million (US$ 780,000).

Geographic entities mentioned:
surface_form: Rímac river
instance_of: Watercourse
countries: Peru
coordinates: lat: -12.032222222222
lon: -77.141111111111
&quot;Sovrompetrol&quot; was followed by &quot;Sovromtransport&quot; and &quot;Tars&quot; (transportation), and later by &quot;Sovrombanc&quot; (banking and commercial monopoly), &quot;Sovromlemn&quot; (wood processing), &quot;Sovromgaz&quot; (natural gas), &quot;Sovromasigurare&quot; (insurance), &quot;Sovromcărbune&quot; (coal exploitation in the Jiu Valley and other areas), &quot;Sovromchim&quot; (chemical industry), &quot;Sovromconstrucţii&quot; (construction materials), &quot;Sovrommetal&quot; (iron mining &mdash; around Reșița), &quot;Sovromtractor&quot; (future ', in Brașov), &quot;Sovromfilm&quot; (importing Soviet cinema productions), &quot;Sovrom Utilaj Petrolier&quot; (producing oil refining equipment) and &quot;Sovromnaval&quot; (shipbuilding in Constanța, Giurgiu, and Brăila).

Geographic entities mentioned:
surface_form: Jiu Valley
instance_of: Valley
countries: Romania
coordinates: lat: 43.77805556
lon: 23.81333333
Tagewaldhorn. The Tagewaldhorn (;) is a mountain in the Sarntal Alps in South Tyrol, Italy.

Geographic entities mentioned:
surface_form: tagewaldhorn
instance_of: Mountain
countries: Italy
coordinates: lat: 46.780555555556
lon: 11.496944444444
Ivar Mortensson-Egnund. Ivar Mortensson-Egnund (originally Ivar Julius Mortensen and also referred to as Ivar Matlaus; 24 July 1857 – 16 February 1934) was a Norwegian author, journalist, theologian, researcher, translator, writer, philosopher and advocate of nynorsk (the new Norwegian language). He was born in Tynset Municipality (now part in Alvdal Municipality) in North Østerdalen.

Geographic entities mentioned:
surface_form: Østerdalen
instance_of: Valley
countries: Norway
coordinates: lat: 61.575916666666664
lon: 11.087111111111112
In 1877 when Garborg started the magazine &quot;Fedraheimen&quot; Mortensson became an employee. It was also Ivar who helped Hulda and Arne Garborg locate & rent a small cabin on the small farm &quot;Kolbotnen&quot;, near the lake Savalen in Alvdal Municipality in 1887. When Garborg moved there, Mortensson followed.

Geographic entities mentioned:
surface_form: Savalen
instance_of: Lake
countries: Norway
coordinates: lat: 62.241111111111
lon: 10.482222222222
Guri i Kuq Lake. The Guri i Kuq Lakes or Liqenet e Kuqishtes (;) are glacial lakes in Kosovo, located on the Guri i Kuq mountain, in the Accursed Mountains range. They are the largest lakes in the Kosovan part of the range after Gjeravica Lake and Liqenat Lake. Unlike Liqenat Lake, the Guri i Kuq lake is not surrounded by trees but instead by large meadows.

Geographic entities mentioned:
surface_form: Guri i Kuq
instance_of: Mountain
countries: Kosovo
coordinates: lat: 42.66265
lon: 20.13343
surface_form: guri i kuq
instance_of: Mountain
countries: Kosovo
coordinates: lat: 42.66265
lon: 20.13343
Guri i Kuq Lake. The Guri i Kuq Lakes or Liqenet e Kuqishtes (;) are glacial lakes in Kosovo, located on the Guri i Kuq mountain, in the Accursed Mountains range. They are the largest lakes in the Kosovan part of the range after Gjeravica Lake and Liqenat Lake. Unlike Liqenat Lake, the Guri i Kuq lake is not surrounded by trees but instead by large meadows.

Geographic entities mentioned:
surface_form: Gjeravica Lake
instance_of: Lake
countries: Kosovo
coordinates: lat: 42.5308
lon: 20.1351
surface_form: liqenat
instance_of: Lake
countries: Kosovo
coordinates: lat: 42.66861111
lon: 20.09083333
surface_form: gjeravica
instance_of: Mountain
countries: Kosovo
coordinates: lat: 42.532777777778
lon: 20.140833333333
The Guri i Kuq Lakes or Liqenet e Kuqishtes (;) are glacial lakes in Kosovo, located on the Guri i Kuq mountain, in the Accursed Mountains range. They are the largest lakes in the Kosovan part of the range after Gjeravica Lake and Liqenat Lake. Unlike Liqenat Lake, the Guri i Kuq lake is not surrounded by trees but instead by large meadows. Just north of the lake is the Rugova Canyon.

Geographic entities mentioned:
surface_form: Rugova Canyon
instance_of: Valley
countries: Kosovo
coordinates: lat: 42.69222222
lon: 20.16861111
Guri i Kuq Lake. The Guri i Kuq Lakes or Liqenet e Kuqishtes (;) are glacial lakes in Kosovo, located on the Guri i Kuq mountain, in the Accursed Mountains range. They are the largest lakes in the Kosovan part of the range after Gjeravica Lake and Liqenat Lake. Unlike Liqenat Lake, the Guri i Kuq lake is not surrounded by trees but instead by large meadows.

Geographic entities mentioned:
surface_form: guri i kuq lake
instance_of: Lake
countries: Kosovo
coordinates: lat: 42.65472222222222
lon: 20.105833333333333
surface_form: guri i kuq
instance_of: Mountain
countries: Kosovo
coordinates: lat: 42.66265
lon: 20.13343
The Guri i Kuq Lakes or Liqenet e Kuqishtes (;) are glacial lakes in Kosovo, located on the Guri i Kuq mountain, in the Accursed Mountains range. They are the largest lakes in the Kosovan part of the range after Gjeravica Lake and Liqenat Lake. Unlike Liqenat Lake, the Guri i Kuq lake is not surrounded by trees but instead by large meadows. Just north of the lake is the Rugova Canyon.

Geographic entities mentioned:
surface_form: guri i kuq lake
instance_of: Lake
countries: Kosovo
coordinates: lat: 42.65472222222222
lon: 20.105833333333333
surface_form: guri i kuq
instance_of: Mountain
countries: Kosovo
coordinates: lat: 42.66265
lon: 20.13343
surface_form: liqenat
instance_of: Lake
countries: Kosovo
coordinates: lat: 42.66861111
lon: 20.09083333
He is a form of Shiva. Origins and significance. According to Partha Sarathi Nath, Sylhet and the Barak Valley were ruled by the Nātha dynasty of nearby Tripura between the twelfth and thirteenth centuries, which promoted the early settlement of Nāthas and their cultural influence in this region.

Geographic entities mentioned:
surface_form: Barak Valley
instance_of: Valley
countries: India
coordinates: lat: 24.833333333333332
lon: 92.8
Ghatshila was earlier the headquarters of the Rajas of Dhalbhum. Ghatshila block was established in 1962 with headquarters at Ghatshila. Geography. “The district forms a part of the Chota Nagpur Plateau and is a hilly upland tract”. The Seraikela Dhalbhumgarh upland and the Dalma range are natural divisions of the district. The main rivers are the Subarnarekha and the Kharkai.

Geographic entities mentioned:
surface_form: Chota Nagpur Plateau
instance_of: Plateau
countries: India
coordinates: lat: 23
lon: 85