Sarmila/GeoWiki-Features huggingface dataset:
Flood, British Columbia. Flood is a rural community in the District of Hope, British Columbia, Canada, located west of the town of Hope on the south bank of the Fraser River in the far eastern end of the Fraser Valley region. It is primarily agricultural in nature. Its official name is Floods, though it is usually referred to by its post office name in the singular, Flood.

Geographic entities mentioned:
surface_form: Fraser Valley
instance_of: Valley
countries: Canada
coordinates: lat: 49.108333333333
lon: -122.29166666667
Chincoteague Inlet. Chincoteague Inlet is found lying between Assateague Island and Wallops Island on the Eastern Shore of Virginia. It is 30 miles south-southwestward from the Ocean City, Maryland Inlet. The approach has no sea buoy, however lighted buoy (R &quot;2&quot;), marking Chincoteague Shoals, is located ESE of the entrance at 37°47’25&quot; N / 075°22’21&quot; W, and can be used.

Geographic entities mentioned:
surface_form: chincoteague inlet
instance_of: Landform
countries: United States
coordinates: lat: 37.88444444
lon: -75.41194444
Prominent on the approach are Assateague Light shown from a 142-foot red and white horizontally banded conical tower and a lookout tower on the southern tip of Assateague Island; both are visible well offshore. The marked channel through the inlet to Chincoteague Channel is subject to frequent change; the buoys are shifted with changing conditions.

Geographic entities mentioned:
surface_form: chincoteague channel
instance_of: Landform
countries: United States
coordinates: lat: 37.91611111
lon: -75.39916667
Nako, Himachal Pradesh. Nako in Spiti river valley is a village in the Himalayas of northern India, located near the close to the India-Tibet border in the Trans-Himalayan region of Kinnaur district in Himachal Pradesh. Nako Lake is a prominent feature here where it borders the village. Nako Monastery, dated to 1025 CE, is located in the village as well as several other Buddhist chortens.

Geographic entities mentioned:
surface_form: Nako Lake
instance_of: Lake
countries: India
coordinates: lat: 31.879638888889
lon: 78.627630555556
Nako Lake is a prominent feature here where it borders the village. Nako Monastery, dated to 1025 CE, is located in the village as well as several other Buddhist chortens. Nako Monastery in the upper part of the village and the Nako Lake are important landmarks in the village. History.

Geographic entities mentioned:
surface_form: Nako Lake
instance_of: Lake
countries: India
coordinates: lat: 31.879638888889
lon: 78.627630555556
Geography. Nako is the largest village in the Hangrang Valley at an elevation of (is also mentioned). The extent of the village is. It is set against the scenic backdrop of Reo Purgyal which has an elevation of and is the highest mountain in Himachal Pradesh. The village is now on a more stable location near the Nako Lake which is formed by the slopes of the mountains of Reo Purgyal.

Geographic entities mentioned:
surface_form: Reo Purgyal
instance_of: Mountain
countries: India
coordinates: lat: 31.884407
lon: 78.735308
The lake has boating facilities during the summer months and ice skating is practiced on the lake's surface which gets frozen during the winter months. Chango gompa. Chango gompa, a few km away from the Nako monastery on the road from Spiti, has a prayer wheel more than 500 years old, which measures about in diameter. It is made of yak skin. Trekking trails.

Geographic entities mentioned:
surface_form: Spiti
instance_of: Valley
countries: India
Qing dynasty
coordinates: lat: 32.246944444444445
lon: 78.05222222222223
Musquaro Lake. The Musquaro Lake is located in the unorganized territory of Petit-Mécatina, Quebec, in the Regional County Municipality (MRC) Le Golfe-du-Saint-Laurent Regional County Municipality, in the administrative area of the Côte-Nord (North-Shore), in Quebec, in Canada. Geography.

Geographic entities mentioned:
surface_form: musquaro lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.5967331
lon: -60.9953364
Geography. Obříství is located about south of Mělník and north of Prague. It lies in a flat landscape in the Central Elbe Table. The municipality is situated on the left bank of the Elbe River. The Vltava River forms the northern municipal border and the confluence of the Elbe and Vltava is located just outside the municipality. History. The first written mention of Obříství is from 1290.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
On March 26, his first encounter with the British Legion, under command of Lieutenant Colonel Banastre Tarleton, resulted in a minor victory near Rantowle's Bridge on the Stono River in South Carolina. Afterward, on the Ashley River during the fight at Rutledge's Plantation on March 26, 1780, Lt. Col. Washington again bested a detachment of Tarleton's dragoons and infantry.

Geographic entities mentioned:
surface_form: Stono River
instance_of: Landform
countries: United States
coordinates: lat: 32.6368
lon: -80.0151
Bras Henriette. The arm Henriette (English: Henriette's arm) is a tributary of the Bras de Jacob, flowing in the southern part of the city of Saguenay, in the administrative region of Saguenay–Lac-Saint-Jean, in the province of Quebec, in Canada. The course of the Henriette arm crosses the northwest part of the zec Mars-Moulin.

Geographic entities mentioned:
surface_form: Bras de Jacob
instance_of: Watercourse
countries: Canada
coordinates: lat: 48.231943
lon: -71.100555
surface_form: saint-jean
instance_of: Lake
countries: Canada
coordinates: lat: 48.594444444444
lon: -72.03
Geography. From the mouth of the Henriette arm, the current successively follows the course of the Bras de Jacob on towards the east, the course of the Rivière du Moulin on to the north, then the course of the Saguenay River on east to Tadoussac where it merges with the Saint Lawrence Estuary. Toponymy. The term &quot;Henriette&quot; is a family name of French origin.

Geographic entities mentioned:
surface_form: Bras de Jacob
instance_of: Watercourse
countries: Canada
coordinates: lat: 48.231943
lon: -71.100555
surface_form: rivière du moulin
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.25056
lon: -72.0225
surface_form: rivière du moulin
instance_of: Watercourse
countries: Canada
coordinates: lat: 45.8778
lon: -70.625
surface_form: rivière du moulin
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.755066666666664
lon: -70.87210277777778
surface_form: rivière du moulin
instance_of: Watercourse
countries: Canada
coordinates: lat: 47.42333194444444
lon: -70.5094438888889
Bras Henriette. The arm Henriette (English: Henriette's arm) is a tributary of the Bras de Jacob, flowing in the southern part of the city of Saguenay, in the administrative region of Saguenay–Lac-Saint-Jean, in the province of Quebec, in Canada. The course of the Henriette arm crosses the northwest part of the zec Mars-Moulin.

Geographic entities mentioned:
surface_form: bras henriette
instance_of: Watercourse
countries: Canada
coordinates: lat: 48.227498888889
lon: -71.124998888889
The course of the Henriette arm crosses the northwest part of the zec Mars-Moulin. The small valley of the Bras Henriette is served by some secondary forest roads, especially for the needs of forestry and recreational tourism activities. Forestry is the main economic activity in this valley; recreational tourism, second.

Geographic entities mentioned:
surface_form: bras henriette
instance_of: Watercourse
countries: Canada
coordinates: lat: 48.227498888889
lon: -71.124998888889
Toponymy. The term &quot;Henriette&quot; is a family name of French origin. The toponym &quot;bras Henriette&quot; was formalized on June 29, 1983, at the Place Names Bank of the Commission de toponymie du Québec.

Geographic entities mentioned:
surface_form: bras henriette
instance_of: Watercourse
countries: Canada
coordinates: lat: 48.227498888889
lon: -71.124998888889
Bear Lodge Mountains. The Bear Lodge Mountains () are a small mountain range in Crook County, Wyoming. These mountains are protected in the Black Hills National Forest as part of its Bearlodge District. Devils Tower National Monument was the first U.S. National Monument and draws about 400,000 visitors per year to the area.

Geographic entities mentioned:
surface_form: Devils Tower National Monument
instance_of: Mountain
countries: United States
coordinates: lat: 44.590277777778
lon: -104.71527777778
Geography. The Bear Lodge Mountains were formed as a byproduct of the geological processes that created the Black Hills, and offer hikes throughout bottomlands, hills, and buttes. Unlike the Black Hills, this range is small and only a few igneous rocks are exposed. Just outside the range, however, lie the very large igneous intrusions of Devils Tower, Inyan Kara Mountain, and Sundance Mountain.

Geographic entities mentioned:
surface_form: Inyan Kara Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.2125
lon: -104.344
Occurrence. Weeksite was first described in 1960 for an occurrence on Topaz Mountain, Thomas Range, Juab County, Utah. Weeksite occurs within small &quot;opal&quot; veins within rhyolite and agglomerates, and as encrustations in sandstones and limestones.

Geographic entities mentioned:
surface_form: Topaz Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.7094
lon: -113.103
Many Greeks remained in Crimea after the Bosporan kingdom fell to the Huns and the Goths, and Chersonesos became part of the Byzantine Empire. Orthodox monasteries continued to function, with strong links with the monasteries of Mount Athos in northern Greece.

Geographic entities mentioned:
surface_form: Mount Athos
instance_of: Mountain
countries: Greece
coordinates: lat: 40.15833333333333
lon: 24.327222222222222
The King of Norway usually visits the river once in the summer to fish. The urban area made up of Bossekop, Elvebakken, and Bukta, also known collectively now as the town of Alta, became a town on 1 January 2000. The population has been growing steadily for many years. On 31 August 2019, a sightseeing helicopter crashed in the mountains of Skoddevarre south of Alta. Government.

Geographic entities mentioned:
surface_form: Skoddevarre
instance_of: Mountain
countries: Norway
coordinates: lat: 69.93583333333333
lon: 23.145833333333332
Geography. Alta Municipality covers, in western Finnmark, mostly situated along the Altafjord, including large tracts of woodlands, as well as parts of the Finnmarksvidda plateau. On its way from the plateau down to the fjord, the river Altaelva has carved out the Sautso canyon, one of the largest canyons in Europe.

Geographic entities mentioned:
surface_form: Finnmarksvidda
instance_of: Plateau
countries: Norway
coordinates: lat: 69.31666667
lon: 23.81666667
Geography. Alta Municipality covers, in western Finnmark, mostly situated along the Altafjord, including large tracts of woodlands, as well as parts of the Finnmarksvidda plateau. On its way from the plateau down to the fjord, the river Altaelva has carved out the Sautso canyon, one of the largest canyons in Europe.

Geographic entities mentioned:
surface_form: Sautso
instance_of: Valley
countries: Norway
coordinates: lat: 69.766592
lon: 23.702939
Alta is based on the mainland of Norway, but it also includes parts of the islands of Stjernøya and Seiland. Seiland is the home of Seiland National Park where the Seilandsjøkelen glacier and the mountain Seilandstuva are located. The highest point in the municipality is the tall mountain &quot;Store Haldi&quot;.

Geographic entities mentioned:
surface_form: Seilandstuva
instance_of: Mountain
countries: Norway
coordinates: lat: 70.446388888889
lon: 23.098055555556
Seiland is the home of Seiland National Park where the Seilandsjøkelen glacier and the mountain Seilandstuva are located. The highest point in the municipality is the tall mountain &quot;Store Haldi&quot;. Several of the notable lakes in Alta include Iešjávri, Juovvajávri, Kovvatnet, and Stuorajávri. In 2020, a landslide destroyed 8 houses. Climate.

Geographic entities mentioned:
surface_form: Iešjávri
instance_of: Lake
countries: Norway
coordinates: lat: 69.6654
lon: 24.209
surface_form: Juovvajávri
instance_of: Lake
countries: Norway
coordinates: lat: 69.8034
lon: 24.0217
Sevier Nunatak. Sevier Nunatak () is a nunatak lying southeast of Richter Peaks, rising to about 1,000 m at the south end of the Walton Mountains, situated in the central portion of Alexander Island, Antarctica. The nunatak was named by the Advisory Committee on Antarctic Names for Lieutenant Commander Moses T. Sevier, U. S. Navy, Assistant Chief of Staff for Supply and Logistics, U. S.

Geographic entities mentioned:
surface_form: Richter Peaks
instance_of: Mountain
coordinates: lat: -71.3333
lon: -70.35
surface_form: sevier nunatak
instance_of: Mountain
coordinates: lat: -71.3667
lon: -70.25
Sevier Nunatak. Sevier Nunatak () is a nunatak lying southeast of Richter Peaks, rising to about 1,000 m at the south end of the Walton Mountains, situated in the central portion of Alexander Island, Antarctica. The nunatak was named by the Advisory Committee on Antarctic Names for Lieutenant Commander Moses T. Sevier, U. S. Navy, Assistant Chief of Staff for Supply and Logistics, U. S.

Geographic entities mentioned:
surface_form: moses
instance_of: Mountain
coordinates: lat: -74.55
lon: -99.1833
Sevier Nunatak. Sevier Nunatak () is a nunatak lying southeast of Richter Peaks, rising to about 1,000 m at the south end of the Walton Mountains, situated in the central portion of Alexander Island, Antarctica. The nunatak was named by the Advisory Committee on Antarctic Names for Lieutenant Commander Moses T. Sevier, U. S. Navy, Assistant Chief of Staff for Supply and Logistics, U. S.

Geographic entities mentioned:
surface_form: sevier nunatak
instance_of: Mountain
coordinates: lat: -71.3667
lon: -70.25
Evciler District. Evciler District is a district of Afyonkarahisar Province of Turkey. Its seat is the town Evciler. Its area is, and its population is 7,183 (2021). The district is near Lake Acıgöl and Işıklı reservoir. The average altitude is.

Geographic entities mentioned:
surface_form: Lake Acıgöl
instance_of: Lake
countries: Turkey
coordinates: lat: 37.8268
lon: 29.8878
Lake Albert (New South Wales). Lake Albert is an artificial lake in the suburb of Lake Albert in Wagga Wagga in New South Wales, Australia. Covering 125 ha, the lake was built in 1868 on what was known as &quot;Swampy Plains&quot; and was named after Prince Albert. Surrounded by parkland, the lake is a venue for water sports, fishing, walking and bird watching.

Geographic entities mentioned:
surface_form: lake albert
instance_of: Lake
countries: Australia
coordinates: lat: -35.61666667
lon: 139.3
surface_form: lake albert (new south wales)
instance_of: Lake
countries: Australia
coordinates: lat: -35.167
lon: 147.373
surface_form: albert
instance_of: Lake
countries: Australia
coordinates: lat: -35.167
lon: 147.373
Lake Albert (New South Wales). Lake Albert is an artificial lake in the suburb of Lake Albert in Wagga Wagga in New South Wales, Australia. Covering 125 ha, the lake was built in 1868 on what was known as &quot;Swampy Plains&quot; and was named after Prince Albert. Surrounded by parkland, the lake is a venue for water sports, fishing, walking and bird watching.

Geographic entities mentioned:
surface_form: lake albert
instance_of: Lake
countries: Australia
coordinates: lat: -35.61666667
lon: 139.3
surface_form: lake albert
instance_of: Lake
countries: Australia
coordinates: lat: -35.61666667
lon: 139.3
surface_form: lake albert
instance_of: Lake
countries: Australia
coordinates: lat: -35.167
lon: 147.373
surface_form: lake albert
instance_of: Lake
countries: Australia
coordinates: lat: -35.167
lon: 147.373
surface_form: albert
instance_of: Lake
countries: Australia
coordinates: lat: -35.167
lon: 147.373
surface_form: albert
instance_of: Lake
countries: Australia
coordinates: lat: -35.167
lon: 147.373
The Barry Carne Memorial Ski Race was held on the second Saturday and Sunday in May of each year, subject to water levels in the lake. On 13 and 14 May 2006 the event returned to Lake Albert after a 4-year absence due to the lake being at record low levels owing to drought but was cancelled in 2007 due to low water levels.

Geographic entities mentioned:
surface_form: lake albert
instance_of: Lake
countries: Australia
coordinates: lat: -35.61666667
lon: 139.3
surface_form: lake albert
instance_of: Lake
countries: Australia
coordinates: lat: -35.167
lon: 147.373
surface_form: albert
instance_of: Lake
countries: Australia
coordinates: lat: -35.167
lon: 147.373
Water levels. Due to years of drought the water level at Lake Albert reached record lows and in 2005 Wagga Wagga City Council considered pumping water into the lake to prevent further fish deaths which was ruled out by a senior council official. After a thunderstorm dumped around in the area the lake reached its full depth in early November 2005.

Geographic entities mentioned:
surface_form: lake albert
instance_of: Lake
countries: Australia
coordinates: lat: -35.61666667
lon: 139.3
surface_form: lake albert
instance_of: Lake
countries: Australia
coordinates: lat: -35.167
lon: 147.373
surface_form: albert
instance_of: Lake
countries: Australia
coordinates: lat: -35.167
lon: 147.373
After a thunderstorm dumped around in the area the lake reached its full depth in early November 2005. In January 2007, a ban on water sport activities on Lake Albert was likely if the lake's water level drops below due to the ongoing drought. On 20 March 2008, the lake was closed for the second time since January 2008 due to high levels of Faecal Coliforms in the water.

Geographic entities mentioned:
surface_form: lake albert
instance_of: Lake
countries: Australia
coordinates: lat: -35.61666667
lon: 139.3
surface_form: lake albert
instance_of: Lake
countries: Australia
coordinates: lat: -35.167
lon: 147.373
surface_form: albert
instance_of: Lake
countries: Australia
coordinates: lat: -35.167
lon: 147.373
Lake Albert (New South Wales). Lake Albert is an artificial lake in the suburb of Lake Albert in Wagga Wagga in New South Wales, Australia. Covering 125 ha, the lake was built in 1868 on what was known as &quot;Swampy Plains&quot; and was named after Prince Albert. Surrounded by parkland, the lake is a venue for water sports, fishing, walking and bird watching.

Geographic entities mentioned:
surface_form: albert
instance_of: Lake
countries: Australia
coordinates: lat: -35.167
lon: 147.373
Monetville is divided into two areas; North Monetville and Monetville. &quot;South&quot; Monetville is generally from Dokis Road south to Bear Lake and Shanty Bay (Baie des Chantiers) of Lake Nipissing. North Monetville extends generally from Dokis Road north to the West Arm of Lake Nipissing and Chapel Island, which Highway 64 crosses on the West Arm.

Geographic entities mentioned:
surface_form: Lake Nipissing
instance_of: Lake
countries: Canada
coordinates: lat: 46.283333333333
lon: -80
Noëlville, originally known as Cosby, was founded in 1905 with the arrival of settlers in the region. Noëlville families travelled by boat, to the south-west end of Lake Nipissing, to establish themselves between Lake Nipissing and the French River. To pay homage to Noël Desmarais, the village's first merchant and the first businessman of the region, the town of Cosby became Noëlville in 1911.

Geographic entities mentioned:
surface_form: Lake Nipissing
instance_of: Lake
countries: Canada
coordinates: lat: 46.283333333333
lon: -80
Matamoros–Brownsville, also known as Brownsville–Matamoros, or simply as the Borderplex, is one of the six transborder agglomerations along the Mexico–United States border. It is part of the Lower Rio Grande Valley region. The city of Matamoros is situated in the Mexican state of Tamaulipas, on the south bank of the Rio Grande, while the city of Brownsville is located in the U.S.

Geographic entities mentioned:
surface_form: Lower Rio Grande Valley region
instance_of: Valley
countries: United States
Mexico
coordinates: lat: 26.22
lon: -98.12
It was plotted from Australian National Antarctic Research Expeditions air photos, and was named by the Antarctic Names Committee of Australia for Leslie Miller, a radio officer at Mawson Station in 1964, and a member of one of the survey parties which carried out a tellurometer traverse passing through the Leckie Range in 1965.

Geographic entities mentioned:
surface_form: miller
instance_of: Mountain
coordinates: lat: -66.0167
lon: -65.2333
surface_form: leckie
instance_of: Mountain
coordinates: lat: -70.4333
lon: 66
surface_form: leslie
instance_of: Mountain
coordinates: lat: -62.5667
lon: -60.2
Leslie Peak. Leslie Peak () is a rock outcrop with a conical peak at its south end, about south of Mount Cook of the Leckie Range, Antarctica.

Geographic entities mentioned:
surface_form: leckie
instance_of: Mountain
coordinates: lat: -70.4333
lon: 66
surface_form: mount cook
instance_of: Mountain
coordinates: lat: -67.91667
lon: 56.46667
surface_form: cook
instance_of: Mountain
coordinates: lat: -67.91667
lon: 56.46667
surface_form: leslie peak
instance_of: Mountain
coordinates: lat: -68
lon: 56.5
surface_form: leslie
instance_of: Mountain
coordinates: lat: -62.5667
lon: -60.2
Leslie Peak. Leslie Peak () is a rock outcrop with a conical peak at its south end, about south of Mount Cook of the Leckie Range, Antarctica.

Geographic entities mentioned:
surface_form: leslie peak
instance_of: Mountain
coordinates: lat: -68
lon: 56.5
surface_form: leslie
instance_of: Mountain
coordinates: lat: -62.5667
lon: -60.2
23rd July Lake. The 23rd July Lake or Benghazi Lake () is a lagoon located between Benghazi's downtown, and the Mediterranean Port of Benghazi. It covers an area of approximately 100 hectares (about 1,000,000 square metres).

Geographic entities mentioned:
surface_form: 23rd july lake
instance_of: Lake
countries: Libya
coordinates: lat: 32.104166666667
lon: 20.063888888889
Big Lake (Grant County, Minnesota). Big Lake is a lake in Grant County, in the U.S. state of Minnesota. Big Lake was named for its relatively large size.

Geographic entities mentioned:
surface_form: big lake
instance_of: Lake
countries: United States
coordinates: lat: 40.0725
lon: -95.345
surface_form: big lake
instance_of: Lake
countries: United States
coordinates: lat: 45.1722398
lon: -67.6821052
surface_form: big lake
instance_of: Lake
countries: United States
coordinates: lat: 45.819722222222
lon: -96.113055555556
Topography. The Vuoksi River flows from Saimaa to Lake Ladoga. Most of the lake is dotted with islands, and narrow channels divide the lake into many parts, each having its own name (major basins include Orivesi, Puruvesi, Haukivesi, Yövesi, Pihlajavesi, and Pyhäselkä, among others).

Geographic entities mentioned:
surface_form: Lake Ladoga
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 60.842777777777776
lon: 31.459722222222222
surface_form: saimaa
instance_of: Lake
countries: Finland
coordinates: lat: 61.25
lon: 28.25
Topography. The Vuoksi River flows from Saimaa to Lake Ladoga. Most of the lake is dotted with islands, and narrow channels divide the lake into many parts, each having its own name (major basins include Orivesi, Puruvesi, Haukivesi, Yövesi, Pihlajavesi, and Pyhäselkä, among others).

Geographic entities mentioned:
surface_form: Orivesi
instance_of: Lake
countries: Finland
coordinates: lat: 62.266666666667
lon: 29.4
surface_form: Puruvesi
instance_of: Lake
countries: Finland
coordinates: lat: 61.833333333333
lon: 29.45
surface_form: Haukivesi
instance_of: Lake
countries: Finland
coordinates: lat: 62.1
lon: 28.433333333333
surface_form: Yövesi
instance_of: Lake
countries: Finland
coordinates: lat: 61.45
lon: 27.4167
surface_form: Pyhäselkä
instance_of: Lake
countries: Finland
coordinates: lat: 62.466666666667
lon: 29.766666666667
surface_form: haukivesi
instance_of: Lake
countries: Finland
coordinates: lat: 61.25
lon: 28.25
Most of the lake is dotted with islands, and narrow channels divide the lake into many parts, each having its own name (major basins include Orivesi, Puruvesi, Haukivesi, Yövesi, Pihlajavesi, and Pyhäselkä, among others). The southernmost major basin is sometimes called &quot;Suur-Saimaa&quot;, or &quot;Greater Saimaa&quot;, but this is not an official name.

Geographic entities mentioned:
surface_form: suur-saimaa
instance_of: Lake
countries: Finland
coordinates: lat: 61.25
lon: 28.25
surface_form: saimaa
instance_of: Lake
countries: Finland
coordinates: lat: 61.25
lon: 28.25
surface_form: saimaa
instance_of: Lake
countries: Finland
coordinates: lat: 61.25
lon: 28.25
surface_form: saimaa
instance_of: Lake
countries: Finland
coordinates: lat: 61.25
lon: 28.25
Saimaa. Saimaa (,;) is a lake located in the Finnish Lakeland area in southeastern Finland. With a surface area of approximately, it is the largest lake in Finland, and the fourth-largest natural freshwater lake in Europe. The name Saimaa likely comes from a non-Uralic, non-Indo European substrate language.

Geographic entities mentioned:
surface_form: saimaa
instance_of: Lake
countries: Finland
coordinates: lat: 61.25
lon: 28.25
With a surface area of approximately, it is the largest lake in Finland, and the fourth-largest natural freshwater lake in Europe. The name Saimaa likely comes from a non-Uralic, non-Indo European substrate language. Alternatively, it has been proposed that the name may be connected to the Sami word &quot;sápmi&quot;. History. The lake was formed by glacial melting at the end of the Ice Age.

Geographic entities mentioned:
surface_form: saimaa
instance_of: Lake
countries: Finland
coordinates: lat: 61.25
lon: 28.25
History. The lake was formed by glacial melting at the end of the Ice Age. Major towns on the lakeshore include Lappeenranta, Imatra, Savonlinna, Mikkeli, Varkaus, and Joensuu. About 6,000 years ago, ancient Lake Saimaa, estimated to cover nearly at the time, was abruptly discharged through a new outlet. The event created thousands of square kilometres of new residual wetlands.

Geographic entities mentioned:
surface_form: saimaa
instance_of: Lake
countries: Finland
coordinates: lat: 61.25
lon: 28.25
surface_form: lake saimaa
instance_of: Lake
countries: Finland
coordinates: lat: 61.25
lon: 28.25
Finland's Ministry for Foreign Affairs describes the Saimaa basin (an area larger than the lake) as a &quot;maze of detail&quot;: according to an English-language statement, the area includes 14,000 islands and &quot;more shoreline here per unit of area than anywhere else in the world, the total length being nearly.&quot;
Natural resources.

Geographic entities mentioned:
surface_form: saimaa
instance_of: Lake
countries: Finland
coordinates: lat: 61.25
lon: 28.25
surface_form: saimaa
instance_of: Lake
countries: Finland
coordinates: lat: 61.25
lon: 28.25
An endangered freshwater seal, the Saimaa ringed seal, lives only at Saimaa. Another of the lake's endangered species is the Saimaa salmon. Due to its rich, easily accessible asbestos deposits, the shores of the lake are the most probable origin of asbestos-ceramic, a type of pottery made between c. 1900 BC – 200 AD.

Geographic entities mentioned:
surface_form: saimaa
instance_of: Lake
countries: Finland
coordinates: lat: 61.25
lon: 28.25
surface_form: saimaa
instance_of: Lake
countries: Finland
coordinates: lat: 61.25
lon: 28.25
Another of the lake's endangered species is the Saimaa salmon. Due to its rich, easily accessible asbestos deposits, the shores of the lake are the most probable origin of asbestos-ceramic, a type of pottery made between c. 1900 BC – 200 AD. The areas around Saimaa lake are a very popular location for summer cabins as well as lake cruises. Saimaa canal.

Geographic entities mentioned:
surface_form: saimaa
instance_of: Lake
countries: Finland
coordinates: lat: 61.25
lon: 28.25
surface_form: saimaa
instance_of: Lake
countries: Finland
coordinates: lat: 61.25
lon: 28.25
1900 BC – 200 AD. The areas around Saimaa lake are a very popular location for summer cabins as well as lake cruises. Saimaa canal. The Saimaa Canal from Lauritsala (Lappeenranta) to Vyborg is 43 kilometres long and connects Saimaa to the Gulf of Finland. Nearly half of the Saimaa Canal runs through a land area leased from Russia.

Geographic entities mentioned:
surface_form: saimaa
instance_of: Lake
countries: Finland
coordinates: lat: 61.25
lon: 28.25
surface_form: saimaa
instance_of: Lake
countries: Finland
coordinates: lat: 61.25
lon: 28.25
The city of McGregor is located just to the south. Marquette itself was originally incorporated as North McGregor in 1874, and it served as a railroad terminus for its southern neighbor. Along with McGregor, the city became a major hub on the railroad, as grain from throughout Iowa and Minnesota was sent through the city en route to Lake Michigan.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Salmon Mountain (California). Salmon Mountain is located in the Klamath Mountains of California and is the highest point in Humboldt County. The area is protected in the Trinity Alps Wilderness on the Six Rivers National Forest.

Geographic entities mentioned:
surface_form: salmon mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.1831
lon: -123.411
Saoura. pb2zp215dy93x78speq33p1b94n12" xml:space="preserve">The Saoura () is a valley in southwestern Algeria. It is formed by the wadi known as Oued Saoura, formed from the confluence of the Oued Guir and Oued Zouzfana at Igli.

Geographic entities mentioned:
surface_form: saoura
instance_of: Valley
countries: Algeria
France
coordinates: lat: 29.45
lon: -1.4333333333333
Näsinneula. Näsinneula (;) is an observation tower in Tampere, Finland, overseeing Lake Näsijärvi. It was built in 1970–1971 and was designed by Pekka Ilveskoski. It is the tallest free-standing structure in Finland and at present the tallest observation tower in the Nordic countries at a height of. The tower opened in 1971 and is located in the Särkänniemi amusement park.

Geographic entities mentioned:
surface_form: Näsijärvi
instance_of: Lake
countries: Finland
coordinates: lat: 61.566666666667
lon: 23.766666666667
Evidence of a traceable Christian Aksumite presence in Amhara dates back to at least the 9th century AD, when the Istifanos monastery was erected on Lake Hayq.

Geographic entities mentioned:
surface_form: Lake Hayq
instance_of: Lake
countries: Ethiopia
coordinates: lat: 11.333333333333
lon: 39.716666666667
On the map of &quot;Historia Aethiopica&quot;, Amhara is situated between the Abay River to the west, the Bashilo River in the north, the Afar Depression to the east and the Awash River to the south. The province consisted of much of Wollo and northern Shewa, and encompassed the region of Lake Hayq and the famous Istifanos Monastery.

Geographic entities mentioned:
surface_form: Lake Hayq
instance_of: Lake
countries: Ethiopia
coordinates: lat: 11.333333333333
lon: 39.716666666667
Law Office & Notary, under the management of Itzhak's son, Yehoshua Nener. Awards and recognition. In 2000, Nener was awarded the Yakir Yerushalayim annual citizenship prize. In September 2017, the Municipality of Jerusalem announced that a street in the city would be named after Itzhak Nener. Death. He died on 27 April 2012. His remains are at Har HaMenuchot, Jerusalem.

Geographic entities mentioned:
surface_form: Har HaMenuchot
instance_of: Mountain
countries: Israel
coordinates: lat: 31.798133333333
lon: 35.177727777778
Mount Thelwood. Mount Thelwood is a mountain on Vancouver Island, British Columbia, Canada, located southeast of Gold River and west of Mount Myra.

Geographic entities mentioned:
surface_form: Mount Myra
instance_of: Mountain
countries: Canada
coordinates: lat: 49.5444
lon: -125.606
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: island
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: mount thelwood
instance_of: Mountain
countries: Canada
coordinates: lat: 49.5389
lon: -125.733
Mount Thelwood. Mount Thelwood is a mountain on Vancouver Island, British Columbia, Canada, located southeast of Gold River and west of Mount Myra.

Geographic entities mentioned:
surface_form: mount thelwood
instance_of: Mountain
countries: Canada
coordinates: lat: 49.5389
lon: -125.733
Ilbesheim bei Landau in der Pfalz. Ilbesheim bei Landau in der Pfalz is a municipality in Südliche Weinstraße district, in Rhineland-Palatinate, western Germany. Geography. Ilbesheim lies on the slopes of the Kleine Kalmit, a hill just outside the Haardt range, southwest of the town of Landau in der Pfalz.

Geographic entities mentioned:
surface_form: Kleine Kalmit
instance_of: Mountain
countries: Germany
coordinates: lat: 49.1862
lon: 8.0574
Vitosha Mountain TV Tower. Vitosha Mountain TV Tower, better known as Kopitoto (, &quot;The Hoof&quot;) after the rock outcrop () it stands on, is a tall TV tower built of reinforced concrete on Vitosha Mountain near Sofia, Bulgaria. The footprint of the tower has the shape of a hexagon with three of the sides extended (i.e. almost triangular).

Geographic entities mentioned:
surface_form: Vitosha
instance_of: Mountain
countries: Bulgaria
coordinates: lat: 42.566666666667
lon: 23.283333333333
Agromyces flavus. &quot;Agromyces flavus&quot; is a Gram-positive, aerobic and non-motile bacterium from the genus of &quot;Agromyces&quot; which has been isolated from soil from the Tibetan Plateau in China.

Geographic entities mentioned:
surface_form: Tibetan Plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 33
lon: 88
Wolchulsan National Park. Wolchulsan National Park () lies in Jeollanam-do province, South Korea. Designated as a national park in 1988, Wolchulsan National Park is South Korea's smallest at only. The park takes its name from Wolchulsan, or Mt. Wolchul in Gangjin and Yeongam counties. The highest peak in the park is Cheong-hwang-bong, with an elevation of.

Geographic entities mentioned:
surface_form: Wolchulsan
instance_of: Mountain
countries: South Korea
coordinates: lat: 34.767777777778
lon: 126.70444444444
The mountain lies about 10 miles northeast of the town of Mill City. Henline Mountain stands 4,644 ft above sea level (1,415 m). The name of the mountain comes from a 19th-century settler. The mountain is most well known for the hike up the mountain which has views of Mt. Jefferson. Henline Mountain shares its name with nearby Henline Falls.

Geographic entities mentioned:
surface_form: jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 44.6743006
lon: -121.799573611
surface_form: mt. jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 44.6743006
lon: -121.799573611
surface_form: mt. jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 45.3522
lon: -68.2828
surface_form: mt. jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 42.4584
lon: -74.6196
surface_form: mt. jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 38.752
lon: -116.927
surface_form: mt. jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 38.0328
lon: -78.5222
surface_form: mt. jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 44.3042
lon: -71.3168
surface_form: mt. jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 42.4918
lon: -72.0395
surface_form: mt. jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 45.6028
lon: -112.006
surface_form: mt. jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 36.403055555556
lon: -81.463333333333
surface_form: mt. jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 44.562
lon: -111.505
Henline Mountain. Henline Mountain is a mountain located in the Opal Creek Wilderness in the Willamette National Forest. The mountain lies about 10 miles northeast of the town of Mill City. Henline Mountain stands 4,644 ft above sea level (1,415 m). The name of the mountain comes from a 19th-century settler. The mountain is most well known for the hike up the mountain which has views of Mt.

Geographic entities mentioned:
surface_form: henline mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.86429
lon: -122.32147
Henline Mountain. Henline Mountain is a mountain located in the Opal Creek Wilderness in the Willamette National Forest. The mountain lies about 10 miles northeast of the town of Mill City. Henline Mountain stands 4,644 ft above sea level (1,415 m). The name of the mountain comes from a 19th-century settler. The mountain is most well known for the hike up the mountain which has views of Mt.

Geographic entities mentioned:
surface_form: henline mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.86429
lon: -122.32147
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
The mountain lies about 10 miles northeast of the town of Mill City. Henline Mountain stands 4,644 ft above sea level (1,415 m). The name of the mountain comes from a 19th-century settler. The mountain is most well known for the hike up the mountain which has views of Mt. Jefferson. Henline Mountain shares its name with nearby Henline Falls.

Geographic entities mentioned:
surface_form: henline mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.86429
lon: -122.32147
Léman (department). Léman () was a department of the French First Republic and French First Empire. Its name came from the French name of Lake Geneva, &quot;Lac Léman&quot;. It was formed in 1798, when the Republic of Geneva was annexed by the French Republic. Léman also included districts that were previously part of the departments of Mont-Blanc (northern Savoy) and Ain (the Pays de Gex).

Geographic entities mentioned:
surface_form: Lake Geneva
instance_of: Lake
countries: Switzerland
France
coordinates: lat: 46.45
lon: 6.55
The Garibaldi Volcanic Belt is a northwest–southeast trending volcanic chain in the Pacific Ranges of the Coast Mountains that extends from Watts Point in the south to the Ha-Iltzuk Icefield in the north. This chain of volcanoes is located in southwestern British Columbia, Canada. It forms the northernmost segment of the Cascade Volcanic Arc, which includes Mount St. Helens and Mount Baker.

Geographic entities mentioned:
surface_form: Mount St. Helens
instance_of: Mountain
countries: United States
coordinates: lat: 46.200277777778
lon: -122.18944444444
surface_form: Mount Baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: mount baker
instance_of: Mountain
countries: Canada
coordinates: lat: 51.665277777777774
lon: -116.59777777777778
Mount Cayley began its formation during this period. Multiple eruptions from 2.2 million to 2,350 years ago created the Mount Meager massif, and eruptions 1.3 million to 9,300 years ago formed Mount Garibaldi and other volcanoes in the Garibaldi Lake area. These major volcanic zones lie in three echelon segments, referred to as the northern, central, and southern segments.

Geographic entities mentioned:
surface_form: Mount Garibaldi
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
lon: -123.00472222222
surface_form: Garibaldi Lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.925
lon: -123.01
surface_form: mount meager
instance_of: Mountain
countries: Canada
coordinates: lat: 50.63166667
lon: -123.50416667
These major volcanic zones lie in three echelon segments, referred to as the northern, central, and southern segments. Each segment contains one of the three major volcanic zones. Apart from these large volcanic zones, two large poorly studied volcanic complexes lie at the northern end of the Pacific Ranges, namely Silverthrone Caldera and Franklin Glacier Complex.

Geographic entities mentioned:
surface_form: Silverthrone Caldera
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4333
lon: -126.3
surface_form: Franklin Glacier Complex
instance_of: Mountain
countries: Canada
coordinates: lat: 51.3333
lon: -125.4
Background. Prior to Garibaldi Belt formation, a number of older, but related volcanic belts were constructed along the Southern Coast of British Columbia. This includes the east–west trending Alert Bay Volcanic Belt on northern Vancouver Island and the Pemberton Volcanic Belt along the coastal mainland.

Geographic entities mentioned:
surface_form: Pemberton Volcanic Belt
instance_of: Mountain
countries: Canada
coordinates: lat: 50.58051944
lon: -122.93235278
surface_form: island
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
In continental rift zones, magma is able to push its way up through the Earth's crust rapidly along faults, providing less chance for differentiation. This is likely the case south of Mount Hood to the California border and east-southeast of the massive Newberry shield volcano adjacent to the Cascade Range in central Oregon because the Brothers Fault Zone lies in this region.

Geographic entities mentioned:
surface_form: Mount Hood
instance_of: Mountain
countries: United States
coordinates: lat: 45.37361111111111
lon: -121.69583333333334
surface_form: Brothers Fault Zone
instance_of: Landform
countries: United States
coordinates: lat: 43.81361111111111
lon: -120.60333333333332
surface_form: mount hood
instance_of: Mountain
countries: Canada
coordinates: lat: 50.75006
lon: -115.08531
Ice-marginal lava flows form when lava erupts from a subaerial vent and ponds against glacial ice. The Barrier, a lava dam impounding Garibaldi Lake in the southern segment, is the best represented ice-marginal lava flow in the Garibaldi Belt. Flow-dominated tuyas and the absence of subglacial fragmental deposits are two uncommon glaciovolcanic features in the Garibaldi chain.

Geographic entities mentioned:
surface_form: Garibaldi Lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.925
lon: -123.01
Southern segment. On the eastern side of Howe Sound lies the southernmost zone of volcanic activity in the Garibaldi chain. This zone, known as the Watts Point volcanic centre, is a small outcrop of volcanic rock that is a portion of a subglacial volcano. The outcrop covers an area of about and an eruptive volume of roughly.

Geographic entities mentioned:
surface_form: Watts Point volcanic centre
instance_of: Mountain
countries: Canada
coordinates: lat: 49.65
lon: -123.21
Successive landslides on Garibaldi's flanks occurred after glacial ice of the Cordilleran Ice Sheet retreated. Subsequent volcanism about 9,300 years ago produced a long dacite lava flow from Opal Cone on Garibaldi's southeastern flank. This is unusually long for a dacite flow, which commonly travel only short distances from a volcanic vent due to their high viscosity.

Geographic entities mentioned:
surface_form: Opal Cone
instance_of: Mountain
countries: Canada
coordinates: lat: 49.8272
lon: -122.971
Before Mount Price was overridden by glacial ice, volcanic activity took place on its northern flank where a satellite vent is present. Renewed activity took place at Clinker Peak on the western flank of Mount Price around 13,000 years ago. This produced the Rubble Creek and Clinker Ridge andesite lava flows that extend to the northwest and southwest.

Geographic entities mentioned:
surface_form: Clinker Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 49.93
lon: -123.04
surface_form: mount price
instance_of: Mountain
countries: Canada
coordinates: lat: 49.9175
lon: -123.03555555555556
It consists of volcanic ash, lapilli and dispersed ropy and lava bomb segments that bring the cone's prominence to. Its minimal degree of erosion indicates that it might have erupted in the past 1,000 years. A series of basaltic andesite flows were erupted from Cinder Cone about 11,000 years ago that traveled into a deep north trending U-shaped valley on the eastern flank of The Black Tusk.

Geographic entities mentioned:
surface_form: The Black Tusk
instance_of: Mountain
countries: Canada
coordinates: lat: 49.97527777777778
lon: -123.04277777777777
surface_form: black tusk
instance_of: Mountain
countries: Canada
coordinates: lat: 49.97527777777778
lon: -123.04277777777777
surface_form: cinder cone
instance_of: Mountain
countries: Canada
coordinates: lat: 49.9717
lon: -123.007
Here, subsequent lava flows from Cinder Cone filled the valley. Central segment. Immediately southeast of Mount Cayley lies Mount Fee, an extensively eroded volcano containing a north–south trending ridge. It is one of the older volcanic features in the central Garibaldi chain.

Geographic entities mentioned:
surface_form: Mount Fee
instance_of: Mountain
countries: Canada
coordinates: lat: 50.0831
lon: -123.25
This volcanic event was also followed by a period of erosion, and likely one or more glacial periods. Extensive erosion following the last volcanic event at Mount Fee has created the rugged north–south trending ridge that currently forms a prominent landmark. Ember Ridge, a volcanic mountain ridge between Tricouni Peak and Mount Fee, consists of at least eight lava domes composed of andesite.

Geographic entities mentioned:
surface_form: Tricouni Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 50.6317
lon: -123.504
surface_form: mount fee
instance_of: Mountain
countries: Canada
coordinates: lat: 50.0831
lon: -123.25
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
After Mount Cayley was constructed, lava flows, tephra and welded dacite rubble were erupted. This second phase of activity million years ago resulted in the creation of the Vulcan's Thumb, a craggy volcanic ridge on the southern flank of Mount Cayley. Lengthy dissection from an extended period of erosion demolished much of the original stratovolcano.

Geographic entities mentioned:
surface_form: Vulcan's Thumb
instance_of: Mountain
countries: Canada
coordinates: lat: 50.11
lon: -123.29
These three volcanic events are in contrast to several others around Cayley in that they do not show signs of interaction with glacial ice. Pali Dome, an eroded volcano north of Mount Cayley, consists of two geological units. Pail Dome East is composed of a mass of andesite lava flows and small amounts of pyroclastic material.

Geographic entities mentioned:
surface_form: Pali Dome
instance_of: Mountain
countries: Canada
coordinates: lat: 50.136944444444
lon: -123.30694444444
This suggests that it erupted less than 10,000 years ago when the regional Fraser Glaciation retreated. Cauldron Dome, a subglacial volcano north of Mount Cayley, lies west of the massive glacier covering much the region. Like Pali Dome, it is composed of two geological units. Upper Cauldron Dome is a flat-topped, oval-shaped pile of at least five andesite lava flows that resembles a tuya.

Geographic entities mentioned:
surface_form: Cauldron Dome
instance_of: Mountain
countries: Canada
coordinates: lat: 50.1556
lon: -123.319
These volcanics were extruded about 10,000 years ago during the waning stages of the Fraser Glaciation from a vent adjacent to upper Cauldron Dome that is currently buried under glacial ice. Lying at the northern portion of the Mount Cayley volcanic field is a subglacial volcano named Slag Hill. At least two geologic units compose the edifice.

Geographic entities mentioned:
surface_form: Slag Hill
instance_of: Mountain
countries: Canada
coordinates: lat: 50.1834
lon: -123.3
surface_form: mount cayley volcanic field
instance_of: Mountain
countries: Canada
coordinates: lat: 50.1203
lon: -123.291