Sarmila/GeoWiki-Features huggingface dataset:
François-Marie Bigex was born at La Balme-de-Thuy, a small town, even then in the Genevois province, set high in the mountains east of Annecy. The family was closely involved with the church. One of his uncles was a priest, as was one of his great-uncles, and the two of them took care of his early schooling. He moved on to attend college at Évian, on the southern shore of the lake.

Geographic entities mentioned:
surface_form: the lake
instance_of: Lake
countries: Switzerland
France
coordinates: lat: 46.45
lon: 6.55
Authorship. During his years of exile beyond the far shore of the lake Bigex also found time to produce and arrange publication of several substantive books intended to address the evils that had befallen the church from the French Revolution and the ensuing Revolutionary Wars.

Geographic entities mentioned:
surface_form: the lake
instance_of: Lake
countries: Switzerland
France
coordinates: lat: 46.45
lon: 6.55
The 2021 roll was 645 students. The school has building has three floors. History. McLaren High School's benefactor and founder was Donald McLaren, a banker, originally from the Strathearn area, the traditional lands of Clan MacLaren. Donald McLaren was born in 1831 and during his lifetime funded and supported the programme that eventually founded McLaren High School in 1892; he died in 1894.

Geographic entities mentioned:
surface_form: Strathearn
instance_of: Valley
countries: United Kingdom
coordinates: lat: 56.3325
lon: -3.6825
With only back-up systems available, the pilots attempt to fly to Innsbruck, Austria, for an emergency landing, but they are losing too much fuel. Metrand realizes they are flying towards a ski area he knows along the Alps in Patscherkofel; they could make a belly landing on a mountain-side. The aircraft approaches the landing site while the ski patrol marks a runway, landing successfully.

Geographic entities mentioned:
surface_form: Patscherkofel
instance_of: Mountain
countries: Austria
coordinates: lat: 47.208611
lon: 11.460556
Mussie. In Canadian folklore, Mussie is a creature said to live in Muskrat Lake in the Canadian province of Ontario. It is variously described, for example, as a walrus or as a three-eyed Loch Ness Monster-like creature.The legend of Mussie likely began around 1916, though legend claims that Canadian pioneer Samuel de Champlain wrote about it in the early seventeenth century.

Geographic entities mentioned:
surface_form: Muskrat Lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.678
lon: -76.908
Characteristics. Mussie's name is a diminutive form of the name of its reported location: Muskrat Lake, a large, deep lake near the village of Cobden, Ontario, and about 75 miles northwest of Ottawa. Muskrat Lake is home to another paranormal phenomenon: local legends state that an Atomic Energy of Canada bus driver saw an extraterrestrial spacecraft landing on a spot atop a hill and leaving.

Geographic entities mentioned:
surface_form: Muskrat Lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.678
lon: -76.908
The name was proposed in 1989 by the Cameroonian linguist Carl Ebobissé. Languages. The A.20 languages are spoken around the Wouri estuary and in the anglophone region around Mount Cameroon. The A.30 languages are spoken along the Atlantic coast of southern Cameroon down to northern Gabon.

Geographic entities mentioned:
surface_form: Wouri estuary
instance_of: Watercourse
countries: Cameroon
coordinates: lat: 3.910154
lon: 9.565544
surface_form: Mount Cameroon
instance_of: Mountain
countries: Cameroon
coordinates: lat: 4.2166666666667
lon: 9.1725
Kashmir division. The Kashmir division is a revenue and administrative division of the Indian-administered Jammu and Kashmir in the disputed Kashmir region. It comprises the Kashmir Valley, bordering the Jammu Division to the south and Ladakh to the east.

Geographic entities mentioned:
surface_form: Kashmir Valley
instance_of: Valley
countries: India
coordinates: lat: 34.0333
lon: 74.6667
Washington Island (Wisconsin). Washington Island is an island of the state of Wisconsin situated in Lake Michigan. Lying about northeast of the tip of the Door Peninsula, it is part of Door County, Wisconsin. The island has a year-round population of 708 people according to the 2010 census.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
These islands form the Town of Washington. Detroit Harbor bay is on the south side of the island. A large part of Washington Island's economy is based on tourism. Washington Island is approximately wide by long. Together with the Door Peninsula, Washington Island forms a treacherous strait that connects Green Bay to the rest of Lake Michigan.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Together with the Door Peninsula, Washington Island forms a treacherous strait that connects Green Bay to the rest of Lake Michigan. Early French explorers named this water way, now littered with shipwrecks, &quot;Porte des Morts&quot;, which literally means &quot;Door of the Dead&quot; or, more colloquially, &quot;Death's Door&quot;, giving both Door County and Door Peninsula their names.

Geographic entities mentioned:
surface_form: Porte des Morts
instance_of: Body of water
countries: United States
coordinates: lat: 45.2933
lon: -86.9586
History. Washington Island is one of a string of islands (which are an outcropping of the Niagara Escarpment) stretching across the entrance of Green Bay from the Door Peninsula in Wisconsin to the Garden Peninsula in Michigan.

Geographic entities mentioned:
surface_form: Niagara Escarpment
instance_of: Mountain
countries: Canada
coordinates: lat: 43.8334
lon: -79.99966
The most common name from after 1650 to 1816 was the Potawatomi Islands. The Potawatomi appear to have first come to especially the southern islands in the string about 1641 (at which time they may figure into the naming of &quot;Porte des Morts&quot;), then left the area for a while, and then returned again and remained there for a considerable length of time.

Geographic entities mentioned:
surface_form: Porte des Morts
instance_of: Body of water
countries: United States
coordinates: lat: 45.2933
lon: -86.9586
These settlers commonly called the whole island by the name of their harbor and in the census of 1850, &quot;Washington Island&quot; appeared. The border between Wisconsin and Michigan was originally defined as &quot;the most usual ship channel&quot; into Green Bay from Lake Michigan but commercial routes existed both to the north and south of the island which led to a border dispute.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
There is one commercial fisherman on the island. Climate. Washington Island has a humid continental climate influenced to some degree by its offshore position in Lake Michigan. This results in summer temperatures being moderated, seasonal lag being prevalent and winters being less cold than in western Wisconsin on the same latitude. Transportation. Washington Island is served by two ferry routes.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
It was given its name by French fur traders, who called it Rivière des Chutes, or &quot;River of the Falls&quot;, a translation of the First Nations name for the site. (The city of Tumwater, founded in the same location, takes its name from the Chinook Jargon translation for &quot;waterfall&quot;.)
Tributaries of the river include Spurgeon Creek, Thurston Creek and Lake Lawrence. Recreation.

Geographic entities mentioned:
surface_form: Lake Lawrence
instance_of: Lake
countries: United States
coordinates: lat: 46.8520415
lon: -122.5710221
Many places in the state have similar Dakota names, such as Minnehaha Falls (&quot;curling water&quot; or waterfall), Minneiska (&quot;white water&quot;), Minneota (&quot;much water&quot;), Minnetonka (&quot;big water&quot;), Minnetrista (&quot;crooked water&quot;), and Minneapolis, a hybrid word combining Dakota ' (&quot;water&quot;) and &quot;-&quot; (Greek for &quot;city&quot;).

Geographic entities mentioned:
surface_form: Minnetonka
instance_of: Lake
countries: United States
coordinates: lat: 44.933333333333
lon: -93.566666666667
The first Europeans to enter the region were French voyageurs, fur traders who arrived in the 17th century. They used the Grand Portage to access trapping and trading areas further into Minnesota. The Anishinaabe (also known as Ojibwe or Chippewa) were migrating into Minnesota, causing tensions with the Dakota people, and dislocated the Mdewakanton from their homelands along Mille Lacs Lake.

Geographic entities mentioned:
surface_form: Mille Lacs Lake
instance_of: Lake
countries: United States
coordinates: lat: 46.2381
lon: -93.6434
The portion of the state east of the Mississippi River became part of the United States at the end of the American Revolutionary War, when the Second Treaty of Paris was signed. Land west of the Mississippi was acquired with the Louisiana Purchase, though the Hudson's Bay Company disputed the Red River Valley until the Treaty of 1818, when the border on the 49th parallel was agreed upon.

Geographic entities mentioned:
surface_form: Red River Valley
instance_of: Valley
countries: Canada
United States
coordinates: lat: 49
lon: -97.5
The state is part of the U.S. region known as the Upper Midwest and part of North America's Great Lakes region. It shares a Lake Superior water border with Michigan and a land and water border with Wisconsin to the east. Iowa is to the south, North Dakota and South Dakota are to the west, and the Canadian provinces of Ontario and Manitoba are to the north.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
There are nearly two dozen rail corridors in Minnesota, most of which go through Minneapolis–St. Paul or Duluth. There is water transportation along the Mississippi River system and from the ports of Lake Superior. Minnesota's principal airport is Minneapolis–St. Paul International Airport (MSP), a major passenger and freight hub for Delta Air Lines and Sun Country Airlines.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
Hallstätter See. Hallstätter See or Lake Hallstatt is a lake in Salzkammergut, Austria. It is named after Hallstatt, a small market town famous for its salt mining since prehistoric times and for being the starting point of the world's oldest still-working industrial pipeline, used to transport brine to Bad Ischl (since 1596) and further to Ebensee.

Geographic entities mentioned:
surface_form: hallstätter see
instance_of: Lake
countries: Austria
coordinates: lat: 47.578611111111
lon: 13.660555555556
The drill is the first time China and Kazakhstan have held anti-terrorism maneuvers. The Collective Security Treaty Organization held exercises in the Caspian Sea simultaneously. The simulation lasted for three days and involved Kazakh forces from border patrol, the Interior Ministry, and the Emergency Situations Ministry, and Chinese law enforcement forces and security services.

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
As the number of settlers increased in Ohio, promoters of the state discussed a proposal for a Miami and Erie Canal to improve transportation to the southwest parts of the state and connect them to markets on and served by Lake Erie. Manor platted the town to prepare for anticipated development.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
Castle Creek (Fraser River tributary). Castle Creek, also known locally as Cottonwood Creek, is a tributary of the Fraser River in the Robson Valley region of British Columbia. Castle Creek flows from its source at Castle Creek glacier in the Cariboo Mountains to its confluence with the Fraser near McBride.

Geographic entities mentioned:
surface_form: Robson Valley
instance_of: Valley
countries: Canada
coordinates: lat: 53.25
lon: -120
Lares trek. The Lares trek is a two- or three-day high-altitude hike in Cusco, Peru, starting near the village Lares, approximately north of Cusco and east of Machu Picchu. The Lares Valley lies in the east of the Urubamba mountain range, traversing part of the Sacred Valley. Reaching the start of the trek requires a bus or van trip of approximately five hours from the village of Lares.

Geographic entities mentioned:
surface_form: Sacred Valley
instance_of: Valley
countries: Peru
coordinates: lat: -13.333333333333
lon: -72.083333333333
The only alternative route north of Wellington to Kapiti and the Manawatu is Transmission Gully which is the route of the four-lane Transmission Gully Motorway. The Gully route was also suggested for the NIMT as part of the proposed Haywards-Plimmerton Line in the 1970s; retaining the existing route as a branch line for commuter traffic to Pukerua Bay or Muri.

Geographic entities mentioned:
surface_form: Transmission Gully
instance_of: Valley
countries: New Zealand
coordinates: lat: -41.05
lon: 174.93
Cocke may have been the first to formulate the Confederate defensive strategy of concentrating forces at Manassas and at Winchester in the Shenandoah Valley, and using the Manassas Gap Railroad to allow them to be mutually supporting. This strategy would be a decisive factor in the Confederate victory in the First Battle of Bull Run.

Geographic entities mentioned:
surface_form: Shenandoah Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.5
lon: -78.85
Tomb of Absalom. The Tomb of Absalom (), also called Absalom's Pillar, is an ancient monumental rock-cut tomb with a conical roof located in the Kidron Valley in Jerusalem, a few metres from the Tomb of Zechariah and the Tomb of Benei Hezir. Although traditionally ascribed to Absalom, the rebellious son of King David of Israel (), recent scholarship has dated it to the 1st century AD.

Geographic entities mentioned:
surface_form: Kidron Valley
instance_of: Valley
countries: State of Palestine
coordinates: lat: 31.776972222222224
lon: 35.23897222222222
Description. Absalom's Pillar is approximately in height. The monument proper stands on a square base and consists of two distinct parts. The lower section is a monolith, hewn out of the rocky slope of the Mount of Olives, while the upper part, rising higher than the original bedrock, is built of neatly cut ashlars.

Geographic entities mentioned:
surface_form: Mount of Olives
instance_of: Mountain
countries: Israel
coordinates: lat: 31.777946
lon: 35.245686
Lake Dardanelle. Lake Dardanelle is a major reservoir on the Arkansas River in Arkansas, USA. and is an integral part of the McClellan-Kerr Arkansas River Navigation System (MKARNS), which allows barge transportation from the Mississippi River to the Tulsa Port of Catoosa in northeastern Oklahoma. MKARNS went into service along its full length in 1971. Lake description.

Geographic entities mentioned:
surface_form: lake dardanelle
instance_of: Lake
countries: United States
coordinates: lat: 35.2833
lon: -93.2333
MKARNS went into service along its full length in 1971. Lake description. Lake Dardanelle, a reservoir on the Arkansas River, provides many recreational opportunities. The lake covers nearly with abundant opportunities for boating, fishing, picnicking, camping and scenic views. The lake extends from Dardanelle Lock and Dam () near Dardanelle, into Pope, Yell, Logan, Johnson and Franklin Counties.

Geographic entities mentioned:
surface_form: lake dardanelle
instance_of: Lake
countries: United States
coordinates: lat: 35.2833
lon: -93.2333
Each recreational park on Dardanelle has drinking water, picnic tables and toilet facilities. Most have trailer dump stations, boat launch ramps and electrical sites. The only nuclear power plant in Arkansas, Arkansas Nuclear One, is located on the northeastern shore of Lake Dardanelle. Mount Nebo (Arkansas) is close to the area and provides scenic views for visitors along the lake.

Geographic entities mentioned:
surface_form: lake dardanelle
instance_of: Lake
countries: United States
coordinates: lat: 35.2833
lon: -93.2333
The mountains of the Ozarks and Ouachitas are abundant in wildlife. The bald eagle often uses this area for wintering. Eagles can be seen here from late fall to early spring. Lake Dardanelle State Park is located on two sites, one in Russellville and the other, across the lake to the south, near Dardanelle.

Geographic entities mentioned:
surface_form: lake dardanelle
instance_of: Lake
countries: United States
coordinates: lat: 35.2833
lon: -93.2333
The only nuclear power plant in Arkansas, Arkansas Nuclear One, is located on the northeastern shore of Lake Dardanelle. Mount Nebo (Arkansas) is close to the area and provides scenic views for visitors along the lake. The Ozark and Ouachita Mountains also offer great scenery and have mountain springs and recreation parks in abundance.

Geographic entities mentioned:
surface_form: mount nebo (arkansas)
instance_of: Mountain
countries: United States
coordinates: lat: 35.2159
lon: -93.2535
The lakes occur in three adjoining local government areas, Beverley, Brookton and Quairading. The lakes, which are a wildlife haven, were often referred to as the County Peak lakes and can be seen from the summit of nearby County Peak. The resultant problems, including salinity issues, have been researched and investigated extensively.

Geographic entities mentioned:
surface_form: County Peak
instance_of: Mountain
countries: Australia
coordinates: lat: -32.1833
lon: 117.167
surface_form: county peak
instance_of: Mountain
countries: Australia
coordinates: lat: -32.1833
lon: 117.167
surface_form: county peak lakes
instance_of: Group of lakes
countries: Australia
coordinates: lat: -32.232777777778
lon: 117.1975
Yenyening Lakes. Yenyenning Lake, also often spelt Yenyening Lakes, and associated lakes are in the upper Avon River catchment area in Western Australia, and the source of the Avon and Swan River systems. It is located in the Wheatbelt region of Western Australia approximately north east of Brookton.

Geographic entities mentioned:
surface_form: yenyening lakes
instance_of: Group of lakes
countries: Australia
coordinates: lat: -32.232777777778
lon: 117.1975
Yenyening Lakes. Yenyenning Lake, also often spelt Yenyening Lakes, and associated lakes are in the upper Avon River catchment area in Western Australia, and the source of the Avon and Swan River systems. It is located in the Wheatbelt region of Western Australia approximately north east of Brookton.

Geographic entities mentioned:
surface_form: yenyening lakes
instance_of: Group of lakes
countries: Australia
coordinates: lat: -32.232777777778
lon: 117.1975
surface_form: yenyenning lake
instance_of: Group of lakes
countries: Australia
coordinates: lat: -32.232777777778
lon: 117.1975
Chandra Parbat I. Chandra Parbat I is a mountain of the Garhwal Himalaya in Uttarakhand, India. Chandra Parbat I stands at. It is 42nd highest located entirely within the Uttrakhand. Nanda Devi, is the highest mountain in this category. Chandra Parbat I lies on the eastern bank of the Suralaya Glacier. It is located between Chandra II (North west) and Chandra III (South).

Geographic entities mentioned:
surface_form: Nanda Devi
instance_of: Mountain
countries: India
coordinates: lat: 30.37388888888889
lon: 79.97083333333333
Nanda Devi, is the highest mountain in this category. Chandra Parbat I lies on the eastern bank of the Suralaya Glacier. It is located between Chandra II (North west) and Chandra III (South). It is located 4.9 km NE of Satopanth and 8 km west lies Vasuki South. On the 7.4 km SWS lies the Swachhand Peak and Bhgirathi Massif on the west side. Climbing History.

Geographic entities mentioned:
surface_form: Satopanth
instance_of: Mountain
countries: India
coordinates: lat: 30.845844
lon: 79.21323
The team members are Darren Miller, Gavin Dunmall, Glen Tempest, James Serie, Peter Williams, Andrew McNeill, Grant Else and Sarah Boyle. They established their Base Camp below Vasuki Parbat and Advance Base at the junction of the Chaturangi and Suralaya Glaciers. They climbed the 70° northwest face to the summit.

Geographic entities mentioned:
surface_form: chaturangi
instance_of: Mountain
countries: India
coordinates: lat: 30.93083333
lon: 79.20694444
surface_form: vasuki parbat
instance_of: Mountain
countries: India
coordinates: lat: 30.875
lon: 79.175277777778
At 5:45 they were on the summit. Glaciers and rivers. It is surrounded by glaciers on both sides Suralaya Glacier on the western side, sweta Bamak on the eastern side. Both glaciers joins with Chaturangi Glacier, and Chaturangi Glacier joins with Gangotri Glacier from there emerges the river Bhagirathi the main tributaries of river Ganga.

Geographic entities mentioned:
surface_form: chaturangi
instance_of: Mountain
countries: India
coordinates: lat: 30.93083333
lon: 79.20694444
surface_form: chaturangi
instance_of: Mountain
countries: India
coordinates: lat: 30.93083333
lon: 79.20694444
Chandra Parbat I. Chandra Parbat I is a mountain of the Garhwal Himalaya in Uttarakhand, India. Chandra Parbat I stands at. It is 42nd highest located entirely within the Uttrakhand. Nanda Devi, is the highest mountain in this category. Chandra Parbat I lies on the eastern bank of the Suralaya Glacier. It is located between Chandra II (North west) and Chandra III (South).

Geographic entities mentioned:
surface_form: chandra parbat
instance_of: Mountain
countries: India
coordinates: lat: 30.85861111111111
lon: 79.255
surface_form: chandra parbat i
instance_of: Mountain
countries: India
coordinates: lat: 30.871744
lon: 79.257216
Chandra Parbat I stands at. It is 42nd highest located entirely within the Uttrakhand. Nanda Devi, is the highest mountain in this category. Chandra Parbat I lies on the eastern bank of the Suralaya Glacier. It is located between Chandra II (North west) and Chandra III (South). It is located 4.9 km NE of Satopanth and 8 km west lies Vasuki South.

Geographic entities mentioned:
surface_form: chandra parbat
instance_of: Mountain
countries: India
coordinates: lat: 30.85861111111111
lon: 79.255
surface_form: chandra parbat i
instance_of: Mountain
countries: India
coordinates: lat: 30.871744
lon: 79.257216
On the 7.4 km SWS lies the Swachhand Peak and Bhgirathi Massif on the west side. Climbing History. An Australian team of eight members climbed the Chandra Parbat I (6739 meters, 22,110 feet) On September 25, 1994. The team members are Darren Miller, Gavin Dunmall, Glen Tempest, James Serie, Peter Williams, Andrew McNeill, Grant Else and Sarah Boyle.

Geographic entities mentioned:
surface_form: chandra parbat
instance_of: Mountain
countries: India
coordinates: lat: 30.85861111111111
lon: 79.255
surface_form: chandra parbat i
instance_of: Mountain
countries: India
coordinates: lat: 30.871744
lon: 79.257216
It is located between Chandra II (North west) and Chandra III (South). It is located 4.9 km NE of Satopanth and 8 km west lies Vasuki South. On the 7.4 km SWS lies the Swachhand Peak and Bhgirathi Massif on the west side. Climbing History. An Australian team of eight members climbed the Chandra Parbat I (6739 meters, 22,110 feet) On September 25, 1994.

Geographic entities mentioned:
surface_form: swachhand
instance_of: Mountain
countries: India
coordinates: lat: 30.809444444444445
lon: 79.22416666666666
NM 186 is also known as West Ohara Road. Route description. The highway begins at the junction with NM 28 south of Chamberino. The road heads east-northeast through pecan orchards and fields of Mesilla Valley and after approximately 0.7 miles crosses La Union Main Canal. At NM 186 passes by Anthony Country Club, then crosses the Rio Grande over a bridge, built in 1957.

Geographic entities mentioned:
surface_form: Mesilla Valley
instance_of: Valley
countries: United States
coordinates: lat: 31.7903
lon: -106.423
WSLS-TV. WSLS-TV (channel 10) is a television station licensed to Roanoke, Virginia, United States, serving the Roanoke–Lynchburg market as an affiliate of NBC. Owned by Graham Media Group, the station maintains studios on Fifth Street in Roanoke, and its transmitter is located on Poor Mountain in Roanoke County. History.

Geographic entities mentioned:
surface_form: Poor Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.1796
lon: -80.1628
This is a relatively solitary formation with the nearest comparable crater being Piazzi Smyth to the northeast. Notable features in the vicinity are the Montes Spitzbergen mountains to the south and the solitary peak Mons Piton to the east-northeast. Kirch is circular and bowl-shaped, with a dark interior having the same albedo as the surrounding terrain. Satellite craters.

Geographic entities mentioned:
surface_form: Montes Spitzbergen
instance_of: Mountain
coordinates: lat: 34.47
lon: -5.21
surface_form: Mons Piton
instance_of: Mountain
coordinates: lat: 40.72
lon: -0.92
[Steiner] was one of Switzerland's outstanding 20th-century photographers. His landscape photographs taken in the Engadine, where he lived and worked for 46 years, are unique on an international as well as a national level. They have had a major influence on an awareness of Switzerland as an unspoiled alpine country of surpassing beauty.

Geographic entities mentioned:
surface_form: the Engadine
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.5497
lon: 9.8959
Religious practices often involved the ritual slaughter of animals or the deposition of metalwork, especially war booty. Weapons and horse trappings have been found in the bog at Llyn Cerrig Bach on Anglesey and are interpreted as votive offerings cast into a lake. Numerous weapons have also been recovered from rivers, especially the Thames but also the Trent and Tyne.

Geographic entities mentioned:
surface_form: Llyn Cerrig Bach
instance_of: Lake
countries: United Kingdom
coordinates: lat: 53.25885
lon: -4.5402888888889
As a result, there is only a small number of Alpine Club huts. Neither are there many cable cars or lifts. There are just two cable cars on the northern perimeter - the Tegelberg and Laber Bergbahn - and three chair lifts: to the Buchenberg, Hörnle and Kolben Saddle. In the central and southern areas there are no lifts or accommodation huts at all.

Geographic entities mentioned:
surface_form: Tegelberg
instance_of: Mountain
countries: Germany
coordinates: lat: 47.5595
lon: 10.7785
Here, although there is still dolomite in smaller areas, the predominant rock is Wetterstein limestone. The Ammergauer Hochplatte and the Säuling are the most impressive mountains made from this rock. In addition, small patches of argillite, marl, sandstones, radiolarite, conglomerates and gravel limestones enrich the landscape.

Geographic entities mentioned:
surface_form: Säuling
instance_of: Mountain
countries: Germany
Austria
coordinates: lat: 47.534722222222
lon: 10.755
Extensive meadow cultivation on calcareous grassland, wet meadows and matgrass meadows further enrich the flora of the Ammergau Alps. Lakes. In the Plansee and the Heiterwanger See the Ammergau Alps have two of the most attractive lakes in the Austrian state of Tyrol. The lakes are located in valleys (a rarity in the Northern Limestone Alps) and cut fjord-like into the forested mountainsides.

Geographic entities mentioned:
surface_form: Heiterwanger See
instance_of: Lake
countries: Austria
coordinates: lat: 47.45833
lon: 10.78056
Lakes. In the Plansee and the Heiterwanger See the Ammergau Alps have two of the most attractive lakes in the Austrian state of Tyrol. The lakes are located in valleys (a rarity in the Northern Limestone Alps) and cut fjord-like into the forested mountainsides. Their shores are almost undeveloped. Other lakes occur on the northwestern edge of the range (the Alpsee, Schwansee and Forggensee). Bogs.

Geographic entities mentioned:
surface_form: Alpsee
instance_of: Lake
countries: Germany
coordinates: lat: 47.551111111111
lon: 10.723611111111
surface_form: Schwansee
instance_of: Lake
countries: Germany
coordinates: lat: 47.5575
lon: 10.719722222222
It has also established a very dense network of forest tracks. In many areas (e.g. on the Friederspitz), intensive grazing of sheep has caused problems as a result of the destruction of grassy alpine mountainside by erosion. Unlike the neighbouring mountain ranges to the west and southwest, the Ammergau Alps only have a few pastures and alms. The majority of the range is covered in forest.

Geographic entities mentioned:
surface_form: Friederspitz
instance_of: Mountain
countries: Germany
coordinates: lat: 47.518333333333
lon: 10.960277777778
The most diverse and touristically interesting part of the Ammergau Alps is in the Hochplatten-Tegelberg Group. Neighbouring mountain ranges. To the north the Ammergau Alps border on the Alpine Foreland. Long distance paths. In the valleys between Unterammergau, Oberammergau, Ettal and Schloss Linderhof there are numerous &quot;loipe&quot;s with a high likelihood of snow in winter.

Geographic entities mentioned:
surface_form: Alpine Foreland
instance_of: Plateau
countries: Germany
coordinates: lat: 48
lon: 12
Fond du Lac Denesuline First Nation. Fond du Lac Dene Nation () is a Dene First Nation located in the boreal forest area of northern Saskatchewan, Canada. The main settlement is Fond-du-Lac, situated on the east side of Lake Athabasca. It is a remote fly-in community. The population in 2011 was 874, mainly of Dene and Métis descent. 705 residents selected Dene as their mother tongue in 2011.

Geographic entities mentioned:
surface_form: Lake Athabasca
instance_of: Lake
countries: Canada
coordinates: lat: 59.266666666667
lon: -109.45
Talish (region). Tālīsh (;;) is a region in the southwestern coast of the Caspian Sea. It is a homeland of the indigenous Talysh people, who inhabit the region and speak the Talysh language. The territory and the language set apart Talish from its neighbors. Talish is now divided between Azerbaijan and Iran.

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
All government ministers of the Talysh-Mugan Autonomous Republic live in exile, in countries such as the Netherlands. Geography. Talish is located in the southwest of the Caspian Sea and stretches to the north for more than 150 kilometers. Talish consisted of the Talysh Mountains and supplemented by a narrow coastal strip.

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
Talish consisted of the Talysh Mountains and supplemented by a narrow coastal strip. High rainfall, dozens of narrow valleys, discharging into the Caspian Sea, or into the Anzali Lagoon, fertile soil and dense vegetation (home of the extinct Caspian tiger) are some geographical features of this land. In the north, Talish merges into the Mugan plain.

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
Gailbach (Drava). Gailbach is a river of East Tyrol, Austria. It is a right tributary the Drava. Its drainage basin is.

Geographic entities mentioned:
surface_form: gailbach
instance_of: Watercourse
countries: Austria
coordinates: lat: 46.745309
lon: 12.483315
Grove Park is also home to the Proctor Creek Greenway Trail. The multi-purpose trail strings together more than 400 acres of greenspace, spanning from Maddox Park along the Beltline Westside Trail all the way to the Chattahoochee River.

Geographic entities mentioned:
surface_form: Chattahoochee River
instance_of: Watercourse
countries: United States
coordinates: lat: 30.7088028
lon: -84.8638097
Comrie, Perth and Kinross. Comrie (;; Pictish: &quot;Aberlednock&quot;; Latin: &quot;Victoria&quot;) is a village and parish in the southern Highlands of Scotland, towards the western end of the Strathearn district of Perth and Kinross, west of Crieff. Comrie is a historic conservation village in a national scenic area along the river Earn.

Geographic entities mentioned:
surface_form: Strathearn
instance_of: Valley
countries: United Kingdom
coordinates: lat: 56.3325
lon: -3.6825
The position of Comrie on the Highland Boundary Fault also gives the village a claim to the contested title of &quot;Gateway to the Highlands&quot;. To the north of the village, Ben Chonzie and the Grampian Mountains rise majestically, while to the south of the village broad open moorland is joined by lesser mountains and glens that provide a wide range of terrain and ecology. History.

Geographic entities mentioned:
surface_form: Ben Chonzie
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.453851
lon: -3.992057
22 acre (c. 9 ha) in size. An infamous battle between the Celts and Romans is known to have occurred on the unidentified mountain Mons Graupius. The area around Comrie, Strathearn, is one of several proposed battle sites. James V of Scotland came to Comrie and Cultybraggan regularly in September to hunt deer. Records survive of the food he consumed included bread, ale and fish sent from Stirling.

Geographic entities mentioned:
surface_form: Strathearn
instance_of: Valley
countries: United Kingdom
coordinates: lat: 56.3325
lon: -3.6825
It originates in the muskeg of north western Alberta, flows west to British Columbia, then curves northward and returns to Alberta, where it follows a north-northeast course towards the Northwest Territories. After passing over two main waterfalls, the Alexandra Falls and Louise Falls, it flows through the town of Hay River and discharges into the Great Slave Lake.

Geographic entities mentioned:
surface_form: Great Slave Lake
instance_of: Lake
countries: Canada
coordinates: lat: 61.666666666667
lon: -114
It is roughly long by 0.3 miles (0.5 km) wide. The hill lies within the town of Branford. The Farm River runs along the west side of the hill and a tributary salt marsh extends around the south and southeast sides. U.S. 1 borders the hill to the north and separates it from Saltonstall Mountain. A small rock quarry (Johnson's Quarry) abandoned in 1942, occupies the south end of the hill.

Geographic entities mentioned:
surface_form: Saltonstall Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.324
lon: -72.8
surface_form: saltonstall mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.324
lon: -72.8
Beacon Hill (Branford, Connecticut). Beacon Hill, (est.) above sea level, is a traprock outcrop located southeast of New Haven, Connecticut overlooking the mouth of the Farm River 1.2 miles north of Long Island Sound.

Geographic entities mentioned:
surface_form: beacon hill
instance_of: Mountain
countries: United States
coordinates: lat: 33.9344
lon: -117.561
surface_form: beacon hill
instance_of: Mountain
countries: United States
coordinates: lat: 41.2718
lon: -72.8582
Beacon Hill (Branford, Connecticut). Beacon Hill, (est.) above sea level, is a traprock outcrop located southeast of New Haven, Connecticut overlooking the mouth of the Farm River 1.2 miles north of Long Island Sound.

Geographic entities mentioned:
surface_form: beacon hill
instance_of: Mountain
countries: United States
coordinates: lat: 33.9344
lon: -117.561
surface_form: beacon hill
instance_of: Mountain
countries: United States
coordinates: lat: 41.2718
lon: -72.8582
surface_form: long island
instance_of: Landform
countries: United States
coordinates: lat: 46.7269
lon: -90.785
It is the southernmost notable summit of the Metacomet Ridge which extends from Long Island Sound near New Haven, Connecticut, north through the Connecticut River Valley of Massachusetts to nearly the Vermont border. Beacon Hill is known for its scenic ledges overlooking a surrounding salt marsh and the greater Sound and for its unique microclimate ecosystems and rare plant communities.

Geographic entities mentioned:
surface_form: beacon hill
instance_of: Mountain
countries: United States
coordinates: lat: 33.9344
lon: -117.561
surface_form: beacon hill
instance_of: Mountain
countries: United States
coordinates: lat: 41.2718
lon: -72.8582
Beacon Hill is known for its scenic ledges overlooking a surrounding salt marsh and the greater Sound and for its unique microclimate ecosystems and rare plant communities. Beacon Hill is traversed by several trails, most notably the Branford Trail. The &quot;Shoreline Trolley Museum&quot; runs trolley service to the base of the hill.

Geographic entities mentioned:
surface_form: beacon hill
instance_of: Mountain
countries: United States
coordinates: lat: 33.9344
lon: -117.561
surface_form: beacon hill
instance_of: Mountain
countries: United States
coordinates: lat: 41.2718
lon: -72.8582
Beacon Hill is traversed by several trails, most notably the Branford Trail. The &quot;Shoreline Trolley Museum&quot; runs trolley service to the base of the hill. Beacon Hill should not be confused with Beacon Hill of New Haven, another traprock hill, to the west. Geography. Beacon Hill rises steeply above the surrounding landscape and (est.) above Long Island Sound.

Geographic entities mentioned:
surface_form: beacon hill
instance_of: Mountain
countries: United States
coordinates: lat: 33.9344
lon: -117.561
surface_form: beacon hill
instance_of: Mountain
countries: United States
coordinates: lat: 41.2718
lon: -72.8582
A small rock quarry (Johnson's Quarry) abandoned in 1942, occupies the south end of the hill. The Metacomet Ridge continues north from Beacon Hill as Saltonstall Mountain. Low outcrops of traprock continue south from the hill to the shore of Long Island Sound and out into the sound as tide-swept rock outcrops and tiny islands. Geology and ecology.

Geographic entities mentioned:
surface_form: beacon hill
instance_of: Mountain
countries: United States
coordinates: lat: 33.9344
lon: -117.561
surface_form: beacon hill
instance_of: Mountain
countries: United States
coordinates: lat: 41.2718
lon: -72.8582
surface_form: saltonstall mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.324
lon: -72.8
The hill formed near the end of the Triassic Period with the rifting apart of the North American continent from Africa and Eurasia. Lava welled up from the rift and solidified into sheets of strata hundreds of feet thick. Subsequent faulting and earthquake activity tilted the strata, creating the cliffs of Beacon Hill.

Geographic entities mentioned:
surface_form: beacon hill
instance_of: Mountain
countries: United States
coordinates: lat: 33.9344
lon: -117.561
surface_form: beacon hill
instance_of: Mountain
countries: United States
coordinates: lat: 41.2718
lon: -72.8582
Hot, dry upper slopes, cool, moist ravines, and mineral-rich ledges of basalt talus produce a combination of microclimate ecosystems on the mountain that support plant and animal species uncommon in greater Connecticut. (See Metacomet Ridge for more information on the geology and ecosystem of Beacon Hill). Conservation and recreation.

Geographic entities mentioned:
surface_form: beacon hill
instance_of: Mountain
countries: United States
coordinates: lat: 33.9344
lon: -117.561
surface_form: beacon hill
instance_of: Mountain
countries: United States
coordinates: lat: 41.2718
lon: -72.8582
Several hiking trails cross the property, most notably the Branford Trail, which loops around the circumference of the town of Branford, passing through a number of scenic conservation areas. &quot;Short Beach&quot;, also a Branford Land Trust property, lies 1 mile (1.6 km) to the south of Beacon Hill along the Branford Trail.

Geographic entities mentioned:
surface_form: beacon hill
instance_of: Mountain
countries: United States
coordinates: lat: 33.9344
lon: -117.561
surface_form: beacon hill
instance_of: Mountain
countries: United States
coordinates: lat: 41.2718
lon: -72.8582
&quot;Short Beach&quot;, also a Branford Land Trust property, lies 1 mile (1.6 km) to the south of Beacon Hill along the Branford Trail. An historic trolley, run by the non-profit Shoreline Trolley Museum, drops hikers and picnickers at a platform at the base of Beacon Hill. The Shoreline Trolley is the oldest running suburban trolley in the United States.

Geographic entities mentioned:
surface_form: beacon hill
instance_of: Mountain
countries: United States
coordinates: lat: 33.9344
lon: -117.561
surface_form: beacon hill
instance_of: Mountain
countries: United States
coordinates: lat: 41.2718
lon: -72.8582
The Shoreline Trolley is the oldest running suburban trolley in the United States. Parking for Beacon Hill and the Branford Trail is located on a cul-de-sac at the end of Dominican Road in Branford, less than 0.25 miles (0.3 km) south of U.S. 1 near the East Haven border.

Geographic entities mentioned:
surface_form: beacon hill
instance_of: Mountain
countries: United States
coordinates: lat: 33.9344
lon: -117.561
surface_form: beacon hill
instance_of: Mountain
countries: United States
coordinates: lat: 41.2718
lon: -72.8582
Beacon Hill, (est.) above sea level, is a traprock outcrop located southeast of New Haven, Connecticut overlooking the mouth of the Farm River 1.2 miles north of Long Island Sound. It is the southernmost notable summit of the Metacomet Ridge which extends from Long Island Sound near New Haven, Connecticut, north through the Connecticut River Valley of Massachusetts to nearly the Vermont border.

Geographic entities mentioned:
surface_form: long island
instance_of: Landform
countries: United States
coordinates: lat: 46.7269
lon: -90.785
surface_form: river valley
instance_of: Valley
countries: United States
coordinates: lat: 35.36
lon: -93.37
The &quot;Shoreline Trolley Museum&quot; runs trolley service to the base of the hill. Beacon Hill should not be confused with Beacon Hill of New Haven, another traprock hill, to the west. Geography. Beacon Hill rises steeply above the surrounding landscape and (est.) above Long Island Sound. It is roughly long by 0.3 miles (0.5 km) wide. The hill lies within the town of Branford.

Geographic entities mentioned:
surface_form: long island
instance_of: Landform
countries: United States
coordinates: lat: 46.7269
lon: -90.785
A small rock quarry (Johnson's Quarry) abandoned in 1942, occupies the south end of the hill. The Metacomet Ridge continues north from Beacon Hill as Saltonstall Mountain. Low outcrops of traprock continue south from the hill to the shore of Long Island Sound and out into the sound as tide-swept rock outcrops and tiny islands. Geology and ecology.

Geographic entities mentioned:
surface_form: long island
instance_of: Landform
countries: United States
coordinates: lat: 46.7269
lon: -90.785
Beacon Hill, open to hiking, picnicking, snowshoeing, bird watching, and other passive pursuits, is isolated from the surrounding suburban areas of Branford and East Haven by salt marsh, riverway, and other wetlands. The hill is steep, with talus slopes in several locations, and offers scenic vistas of Long Island Sound and protected salt marsh from a number of outlooks.

Geographic entities mentioned:
surface_form: long island
instance_of: Landform
countries: United States
coordinates: lat: 46.7269
lon: -90.785
This chain includes some remarkable peaks, mainly Capu Ladroncellu (2145 m), Monte Corona (2144 meters), the Capu a u Dente (2025 meters), Punta Radich (2012 m), Monte Grosso (1937 meters) and San Parteo, and form a large part of the casket of Giunssani. Until 1935, an Easter Monday procession took place in a chapel, now in ruins, situated at altitude in the San Parteo.

Geographic entities mentioned:
surface_form: Monte Grosso
instance_of: Mountain
countries: France
coordinates: lat: 42.5
lon: 8.9166666666667
surface_form: san parteo
instance_of: Mountain
countries: France
coordinates: lat: 42.51944444
lon: 8.96416667
San Parteo. Monte San Parteo (Corsican: San Parteu) is a mountain peak located in Monticello, Haute-Corse, Corsica. Situated between the valley of the River Melaja Tartagine and the valley of Fiume di Regino, the mountain rises to. It is part of the Monte Cinto massif. San Parteo straddles the communes of Pioggiola and Feliceto.

Geographic entities mentioned:
surface_form: monte cinto
instance_of: Mountain
countries: France
coordinates: lat: 42.37972222222222
lon: 8.945833333333333
San Parteo. Monte San Parteo (Corsican: San Parteu) is a mountain peak located in Monticello, Haute-Corse, Corsica. Situated between the valley of the River Melaja Tartagine and the valley of Fiume di Regino, the mountain rises to. It is part of the Monte Cinto massif. San Parteo straddles the communes of Pioggiola and Feliceto.

Geographic entities mentioned:
surface_form: san parteo
instance_of: Mountain
countries: France
coordinates: lat: 42.51944444
lon: 8.96416667
San Parteo. Monte San Parteo (Corsican: San Parteu) is a mountain peak located in Monticello, Haute-Corse, Corsica. Situated between the valley of the River Melaja Tartagine and the valley of Fiume di Regino, the mountain rises to. It is part of the Monte Cinto massif. San Parteo straddles the communes of Pioggiola and Feliceto.

Geographic entities mentioned:
surface_form: san parteo
instance_of: Mountain
countries: France
coordinates: lat: 42.51944444
lon: 8.96416667
surface_form: san parteu
instance_of: Mountain
countries: France
coordinates: lat: 42.51944444
lon: 8.96416667
Situated between the valley of the River Melaja Tartagine and the valley of Fiume di Regino, the mountain rises to. It is part of the Monte Cinto massif. San Parteo straddles the communes of Pioggiola and Feliceto. It is part of a mountain range that marks both the entire northwestern part of the Regional Natural Park of Corsica and the western part of Giunssani.

Geographic entities mentioned:
surface_form: san parteo
instance_of: Mountain
countries: France
coordinates: lat: 42.51944444
lon: 8.96416667
This chain includes some remarkable peaks, mainly Capu Ladroncellu (2145 m), Monte Corona (2144 meters), the Capu a u Dente (2025 meters), Punta Radich (2012 m), Monte Grosso (1937 meters) and San Parteo, and form a large part of the casket of Giunssani. Until 1935, an Easter Monday procession took place in a chapel, now in ruins, situated at altitude in the San Parteo.

Geographic entities mentioned:
surface_form: san parteo
instance_of: Mountain
countries: France
coordinates: lat: 42.51944444
lon: 8.96416667
Until 1935, an Easter Monday procession took place in a chapel, now in ruins, situated at altitude in the San Parteo. The chapel was dedicated to Saint Parthée (San Parteu), a fifth-century saint who was very popular in the Giunssani. Although not the highest, the San Parteo is not easily accessible. Some take a path from Feliceto, but this route has become notorious because of large landslides.

Geographic entities mentioned:
surface_form: san parteo
instance_of: Mountain
countries: France
coordinates: lat: 42.51944444
lon: 8.96416667
Until 1935, an Easter Monday procession took place in a chapel, now in ruins, situated at altitude in the San Parteo. The chapel was dedicated to Saint Parthée (San Parteu), a fifth-century saint who was very popular in the Giunssani. Although not the highest, the San Parteo is not easily accessible. Some take a path from Feliceto, but this route has become notorious because of large landslides.

Geographic entities mentioned:
surface_form: san parteu
instance_of: Mountain
countries: France
coordinates: lat: 42.51944444
lon: 8.96416667
Mica itself is located on the northern edge of the Palouse farming region, with its gentle rolling hills quickly giving way to the foothills of the Selkirk Mountains. Krell Hill, known locally as Tower Mountain for the television towers it houses, is located just to the northwest of town and Mica Peak just to the east.

Geographic entities mentioned:
surface_form: Krell Hill
instance_of: Mountain
countries: United States
coordinates: lat: 47.3446
lon: -117.175