Sarmila/GeoWiki-Features huggingface dataset:
Ettersgill is a village in County Durham, England. It is situated at the top of Teesdale, on the north side of the Tees between Newbiggin and Forest-in-Teesdale, and is in the civil parish of Forest and Frith. The village consists of scattered farms and farmhouses, centered on the fertile valley created by Etters Gill Beck, which flows from the moorland into the Tees south of High Force.

Geographic entities mentioned:
surface_form: Teesdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.545
lon: -1.927
Geography. Opatovice nad Labem is located about north of Pardubice and south of Hradec Králové. It lies in a flat landscape of the East Elbe Table lowland. It is situated on the right bank of the Elbe River. There are several flooded quarries used for recreational purposes. The largest of them is Opaťák in the northern part of the municipality. The Opatovice Canal flows through the village.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
Andinoacara latifrons. &quot;Andinoacara latifrons&quot;, the platinum acara, is a species of fish in the family Cichlidae in the order Perciformes, native to the Magdalena, Atrato, Sinú, and San Juan River basins in Colombia. The scientific species name is indicative to its looks; &quot;latifrons&quot; meaning &quot;broad forehead&quot; or &quot;broad front&quot; in Latin. Description.

Geographic entities mentioned:
surface_form: Sinú
instance_of: Watercourse
countries: Colombia
coordinates: lat: 8.75825
lon: -75.88811111111112
Later life. Ismailciuc retired in 1965 to become a coach for Dinamo Bucharest, and for the rest of his life remained an advisor to many Romanian canoeists and coaches. He died in 1986 in the house he had built for himself on the shore of Lake Snagov near Bucharest.

Geographic entities mentioned:
surface_form: Lake Snagov
instance_of: Lake
countries: Romania
Socialist Republic of Romania
Romanian People's Republic
Principality of Wallachia
Kingdom of Romania
United Principalities of Moldavia and Wallachia
coordinates: lat: 44.73
lon: 26.18
But this restriction was systematically violated, so the reclamation programs constituted huge subsidies to the biggest growers and enabled them to squeeze out small farmers. In 1944, Taylor led opposition to the insertion of an exemption from the limitation into the U.S. Senate bill authorizing the Central Valley Project to bring water into the San Joaquin Valley.

Geographic entities mentioned:
surface_form: San Joaquin Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.628888888889
lon: -120.185
Twin Glacier. Twin Glacier is a glacier in northwestern British Columbia, Canada, located on the northern and eastern flanks of Hoodoo Mountain. It lies at the headwaters of the Twin River. The glacier originates from the Andrei Icefield.

Geographic entities mentioned:
surface_form: Hoodoo Mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 56.772222222222
lon: -131.29444444444
Twin Glacier. Twin Glacier is a glacier in northwestern British Columbia, Canada, located on the northern and eastern flanks of Hoodoo Mountain. It lies at the headwaters of the Twin River. The glacier originates from the Andrei Icefield.

Geographic entities mentioned:
surface_form: Twin River
instance_of: Watercourse
countries: Canada
coordinates: lat: 56.72361111
lon: -131.21166667
Furthermore the villagers of Saleh Khana still wear their turbans and grow their moustache like Afridis, customs which have been passed down by the elders. Geography. Tirah comprises an area of some six to seven hundred square miles and includes under this general name all the valleys lying round the source of the Bara River. The five chief valleys are Maidan, Rajgul, Waran, Bara and Mastura.

Geographic entities mentioned:
surface_form: Bara River
instance_of: Watercourse
countries: Pakistan
coordinates: lat: 34.1
lon: 71.75
The Mastura Valley occupies the southern half of Tirah, and is inhabited by the Orakzais. It is one of the prettiest valleys on the frontier, lying at an elevation of. The Orakzais live, for the most part, in the Miranzai Valley, in the winter, and retreat to Mastura, like the Afridis, during the summer months.

Geographic entities mentioned:
surface_form: Miranzai Valley
instance_of: Valley
countries: Pakistan
On March 24, 1537, the Spanish, under the command of Gonzalo Jiménez de Quesada, took possession of the town. In 1781, during the Revolt of the Comuneros, the march of the insurgents towards Bogotá stopped near Chía in order to cross the Bogotá River, in what is now known as the Bridge of the Commoners (). At that site, the viceroy signed a series of concessions to the rebels.

Geographic entities mentioned:
surface_form: Bogotá River
instance_of: Watercourse
countries: Colombia
coordinates: lat: 5.25
lon: -73.666666666667
On the night of September 28–29 this force of two rifle regiments with tank and artillery support attacked positions held by the 1st Romanian Infantry Division south of Lake Sarpa, driving them back as much as 5 km and liberating the villages of Tsatsa and Simkin by October 1. This was an ominous foretaste of the weakness of the Romanian forces north and south of Stalingrad.

Geographic entities mentioned:
surface_form: Lake Sarpa
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 48.357777777778
lon: 44.629166666667
The Swedish–Russian Arc-of-Meridian expedition was a scientific expedition to Svalbard that took place from 1899 to 1902. The main purpose of the mission was to measure a meridian arc, in order to determine the earth flattening at the poles. The measurements were done by establishing a chain of triangulation points from Keilhaufjellet in Sørkapp Land to Vesle Tavleøya north of Nordaustlandet.

Geographic entities mentioned:
surface_form: Keilhaufjellet
instance_of: Mountain
countries: Norway
coordinates: lat: 76.6285
lon: 16.9032
Alkali Lakes (California). The Alkali Lakes are a series of three large playas located in the Surprise Valley of northeastern California, United States. From north to south they are known as Upper, Middle and Lower Alkali Lake. Upper Alkali Lake is often known simply as Upper Lake, and Lower Alkali Lake as Lower Lake.

Geographic entities mentioned:
surface_form: Surprise Valley
instance_of: Valley
countries: United States
coordinates: lat: 41.5292
lon: -120.173
surface_form: alkali lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 41.43861111
lon: -120.0575
Alkali Lakes (California). The Alkali Lakes are a series of three large playas located in the Surprise Valley of northeastern California, United States. From north to south they are known as Upper, Middle and Lower Alkali Lake. Upper Alkali Lake is often known simply as Upper Lake, and Lower Alkali Lake as Lower Lake.

Geographic entities mentioned:
surface_form: alkali lakes (california)
instance_of: Group of lakes
countries: United States
coordinates: lat: 41.43861111
lon: -120.0575
Prior to European settlement, the area was inhabited by the Kidütökadö, a band of the Northern Paiute. The town of Fort Bidwell is located at the north end of Upper Alkali Lake. Lake City and Cedarville are located between and west of Upper and Middle Alkali Lakes. Eagleville is situated south of Lower Alkali Lake. California State Route 299 crosses the basin in-between the Upper and Middle lakes.

Geographic entities mentioned:
surface_form: alkali lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 41.43861111
lon: -120.0575
The total catchment of Middle Alkali Lake is. Creeks flowing into the lake include Sand, Fortymile, Cedar, Deep, Granger, Milk, Cottonwood, Owl and Raider Creeks. Between Middle and Lower Alkali Lakes there is a smaller lake called Cambron Lake, fed by Highrock and Eagle Creeks. Lower Alkali Lake. Lower Alkali Lake is the southernmost and smallest lake, draining.

Geographic entities mentioned:
surface_form: alkali lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 41.43861111
lon: -120.0575
Spessartskopf. Spessartskopf is an Odenwald mountain in Hesse, Germany.

Geographic entities mentioned:
surface_form: spessartskopf
instance_of: Mountain
countries: Germany
coordinates: lat: 49.6172
lon: 8.87472
Breadalbane Hydro-Electric Scheme. The Breadalbane Hydro-Electric Scheme is a hydroelectric scheme in the Breadalbane area of Perthshire, Scotland. It comprises seven power stations which generate 120MW of power from the dams around Loch Lyon, Loch Earn and Loch Tay. History.

Geographic entities mentioned:
surface_form: Loch Lyon
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.540449
lon: -4.580667
surface_form: Loch Earn
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.385733
lon: -4.20378
surface_form: Loch Tay
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.515555555556
lon: -4.1461111111111
This was a fairly small loch, but its level was raised by, enabling it to store of water. From the dam, a tunnel and pipeline feeds the water to Finlarig power station, located on the shore of Loch Tay at its south-western end. Finlarig contains a single 30 MW Pelton turbine generating set, which is the largest Pelton turbine in Britain. The dam is long and tall at its highest point.

Geographic entities mentioned:
surface_form: Loch Tay
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.515555555556
lon: -4.1461111111111
To increase the amount of water available, the headwaters of streams that fed into Loch Tay, the River Lyon and the River Lochay were captured by a series of tunnels and aqueducts, increasing its catchment area to. Additionally, headwaters from two tributaries of the River Lochay are fed directly into the tunnel supplying the power station.

Geographic entities mentioned:
surface_form: River Lyon
instance_of: Valley
countries: United Kingdom
coordinates: lat: 56.59864
lon: -4.25283
His name (Noochickoneh) first appears as a chief's signature to a letter to Governor Patrick Gordon in June 1732, sent in explanation for the sudden move of Shawnees from Pechoquealin (now Smithfield Township, Monroe County, Pennsylvania) to Wyomink in August, 1728. The move was so sudden that the Shawnees did not take the time to harvest their cornfields.

Geographic entities mentioned:
surface_form: Wyomink
instance_of: Valley
countries: United States
coordinates: lat: 41.251
lon: -75.906
Neucheconeh shared leadership of the Pennsylvania Shawnee with Kakowatcheky until 1745. Treaty with Thomas Penn, 1739. On 27 July 1739, Cacowatchike (Kakowatcheky), Newcheconneh, Tamenebuck, and Meshemethequater came to Philadelphia from Wyoming and Allegheny to hold a council with Governor Thomas Penn.

Geographic entities mentioned:
surface_form: Wyoming
instance_of: Valley
countries: United States
coordinates: lat: 41.251
lon: -75.906
A new treaty was concluded at this council, in which it was declared that the Shawnees had moved to the Allegheny from their former home on the Susquehanna. This treaty was signed on behalf of the Shawnees on the Juniata River and Susquehanna River by Kaycowockewr (Kakowatcheky), chief of those at Wyoming Valley, and by Newcheconner and Tomenebuck, for the Shawnees of Allegheny.

Geographic entities mentioned:
surface_form: Wyoming Valley
instance_of: Valley
countries: United States
coordinates: lat: 41.251
lon: -75.906
Conflicts with the English traders on the Allegheny prompted Kakowatcheky himself to move to Logstown in 1744. Association with Peter Chartier, 1745-1748. About 1730, the Shawnees from Opessa's Town on the Potomac (now Oldtown, Maryland) moved to the Allegheny, and they were followed during the next four years by most of the Pekowi Shawnees then living in the Cumberland Valley.

Geographic entities mentioned:
surface_form: Cumberland Valley
instance_of: Valley
countries: United States
coordinates: lat: 39.93
lon: -77.72
Grono set up a base in a cove on the south coast of Secretary Island; the site is still known as Grono Bay. The Highest peak on Secretary Island is named Mount Grono, and at least one old chart names the sound itself &quot;Gronow's&quot; instead of &quot;Doubtful&quot;. In the upper sound lies Elizabeth Island, which Grono named for his wife.

Geographic entities mentioned:
surface_form: Mount Grono
instance_of: Mountain
countries: New Zealand
coordinates: lat: -45.266
lon: 166.952
History. Before European settlers arrived in Lemont, Native Americans traveled the Des Plaines River in birch bark canoes on trading trips between the Mississippi River and Lake Michigan. The native Potawatomi lived off the land in this area, directly using natural resources for food, shelter, clothing and medicine.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
When it was completed in 1848, it provided a continuous waterway stretching from New York (through the Erie Canal, Lake Erie, Lake Huron and Lake Michigan to Chicago, then through the I&M Canal for entering the Illinois River at LaSalle, Illinois, to the Mississippi River, to New Orleans) to the Gulf of Mexico.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
Ludaš Lake. Ludaš or Ludoš Lake (Serbian: Ludaško / Ludoško jezero; Hungarian: Ludas or Ludasi-tó) is a shallow lake in the province of Vojvodina in northern Serbia, near the city of Subotica. It is a special natural preserve and, since 1977, designated as a swamp area of international significance by the Ramsar Convention.

Geographic entities mentioned:
surface_form: ludoško jezero
instance_of: Lake
countries: Serbia
coordinates: lat: 46.1
lon: 19.82
surface_form: ludas
instance_of: Lake
countries: Serbia
coordinates: lat: 46.1
lon: 19.82
Ludaš Lake. Ludaš or Ludoš Lake (Serbian: Ludaško / Ludoško jezero; Hungarian: Ludas or Ludasi-tó) is a shallow lake in the province of Vojvodina in northern Serbia, near the city of Subotica. It is a special natural preserve and, since 1977, designated as a swamp area of international significance by the Ramsar Convention.

Geographic entities mentioned:
surface_form: ludaš lake
instance_of: Lake
countries: Serbia
coordinates: lat: 46.1
lon: 19.82
Ludaš or Ludoš Lake (Serbian: Ludaško / Ludoško jezero; Hungarian: Ludas or Ludasi-tó) is a shallow lake in the province of Vojvodina in northern Serbia, near the city of Subotica. It is a special natural preserve and, since 1977, designated as a swamp area of international significance by the Ramsar Convention. The name of the lake stems from Hungarian &quot;ludas&quot;, meaning goose. Geography.

Geographic entities mentioned:
surface_form: ludas
instance_of: Lake
countries: Serbia
coordinates: lat: 46.1
lon: 19.82
Distribution and habitat. Their range extends from Tillas Slough at the mouth of the Smith River in Del Norte County, California, south to Agua Hedionda Lagoon in San Diego County. While once recorded in at least 87 coastal locations, they are now gone from many, including San Francisco Bay, although they can still be found nearby at Rodeo Lagoon in Marin County and in San Pedro Creek in Pacifica.

Geographic entities mentioned:
surface_form: Rodeo Lagoon
instance_of: Lake
countries: United States
coordinates: lat: 37.8308
lon: -122.531
Stenhousemuir. Stenhousemuir (;) is a town in the Central Lowlands of Scotland. It lies within the Falkirk council area of Scotland. The town is north-northwest of Falkirk and directly adjoins to Larbert in the west, where the nearest rail access is located. The villages of Carron and Carronshore adjoin Stenhousemuir to the east but to a lesser extent.

Geographic entities mentioned:
surface_form: Central Lowlands
instance_of: Valley
countries: United Kingdom
coordinates: lat: 56.408
lon: -4.044
Alachua culture villages budded off to form clusters connected by a series of forest trails, many of which are still in use as paved roads; among these clusters are some in the present city limits of Gainesville near the Devil's Millhopper and near Moon Lake (the eastern shore of which is from the city limits) as well as northwest of and north-central of Paynes Prairie, and west of Newnans Lake.

Geographic entities mentioned:
surface_form: Newnans Lake
instance_of: Lake
countries: United States
coordinates: lat: 29.650688888889
lon: -82.218333333333
Hogtown is the eponymous village of the adjacent Hogtown Creek, which flows through Gainesville. Hogtown continued to exist until after Gainesville was founded, as evidenced on a map showing both towns, which was published in 1864 based on surveys from 1855. Two residents of Hogtown played a prominent role in establishing Gainesville.

Geographic entities mentioned:
surface_form: Hogtown Creek
instance_of: Watercourse
countries: United States
coordinates: lat: 29.64719
lon: -82.37511
Most notably there you can see a difference between the tourist islands which suffer more anthropocentric change and others which do not. There are also some islands more isolated or protected from the effects of weather in the Bay of Bengal. Tarmugli, the largest island, is covered with thick mangrove vegetation, sand covered beaches, uprooted trees and sheet rocks.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
For decades speculative theories of their natural origin were proposed, but no detailed study was conducted. In 2015 geologists from UC Berkeley concluded that the formations are the result of snowmelt seeping down into volcanic ash from the catastrophic eruption of the Long Valley Caldera, then rising up again as steam.

Geographic entities mentioned:
surface_form: Long Valley Caldera
instance_of: Landform
countries: United States
coordinates: lat: 37.716666666667
lon: -118.88416666667
Yalu River. The Yalu River () or Amnok River () is a river on the border between China and North Korea. Together with the Tumen River to its east, and a small portion of Paektu Mountain, the Yalu forms the border between China and North Korea. Its valley has been the scene of several military conflicts in the past centuries. It borders North Korea to the south and China to the north. Name.

Geographic entities mentioned:
surface_form: Paektu Mountain
instance_of: Mountain
countries: North Korea
People's Republic of China
coordinates: lat: 41.992777777778
lon: 128.07722222222
Geography. From above sea level on Paektu Mountain on the China–North Korea border, the river flows south to Hyesan before sweeping north-west to Linjiang and then returning to a more southerly route for a further to empty into Korea Bay between Dandong (China) and Sinuiju (North Korea).

Geographic entities mentioned:
surface_form: Paektu Mountain
instance_of: Mountain
countries: North Korea
People's Republic of China
coordinates: lat: 41.992777777778
lon: 128.07722222222
The shores of the lake are steep in the western and southern stretches and gently sloping in the remaining perimeter. The slopes of high Burkitty Mountain rise beyond the western lakeshore. Among the lakes in its vicinity, Kotyrkol lies to the SSE, small lake Kotyrkol to the northwest, Balytkty to the WSW, Shchuchye to the WNW and Mamay to the southeast. Flora and fauna.

Geographic entities mentioned:
surface_form: mamay
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 52.55833333
lon: 71.21694444
surface_form: kotyrkol
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 52.9625
lon: 70.413055555556
surface_form: kotyrkol
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 52.9625
lon: 70.413055555556
It lies at an elevation of. It has a roughly round shape, quite regular on the eastern part. The Sarymsak river flows into the lake from the north. In years of abundant water it may flow out from the southeast, connecting Zhokey with neighboring lake Kotyrkol. The shores of the lake are steep in the western and southern stretches and gently sloping in the remaining perimeter.

Geographic entities mentioned:
surface_form: kotyrkol
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 52.9625
lon: 70.413055555556
surface_form: zhokey
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 52.89306
lon: 70.58306
Zhokey. Zhokey (), also known as Zhukey (), is a salt lake in Birzhan sal District, Akmola Region, Kazakhstan. The villages of Zhukey, Karlovka, and Kyzyluyum are located by the lakeshore. Stepnyak town, the district capital, lies to the ESE. Geography. Zhokey lies at the northern end of the Kazakh Uplands and is part of the Irtysh basin. It lies at an elevation of.

Geographic entities mentioned:
surface_form: zhokey
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 52.89306
lon: 70.58306
Zhokey. Zhokey (), also known as Zhukey (), is a salt lake in Birzhan sal District, Akmola Region, Kazakhstan. The villages of Zhukey, Karlovka, and Kyzyluyum are located by the lakeshore. Stepnyak town, the district capital, lies to the ESE. Geography. Zhokey lies at the northern end of the Kazakh Uplands and is part of the Irtysh basin. It lies at an elevation of.

Geographic entities mentioned:
surface_form: zhokey
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 52.89306
lon: 70.58306
surface_form: zhukey
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 52.89306
lon: 70.58306
The villages of Zhukey, Karlovka, and Kyzyluyum are located by the lakeshore. Stepnyak town, the district capital, lies to the ESE. Geography. Zhokey lies at the northern end of the Kazakh Uplands and is part of the Irtysh basin. It lies at an elevation of. It has a roughly round shape, quite regular on the eastern part. The Sarymsak river flows into the lake from the north.

Geographic entities mentioned:
surface_form: zhokey
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 52.89306
lon: 70.58306
Zhokey. Zhokey (), also known as Zhukey (), is a salt lake in Birzhan sal District, Akmola Region, Kazakhstan. The villages of Zhukey, Karlovka, and Kyzyluyum are located by the lakeshore. Stepnyak town, the district capital, lies to the ESE. Geography. Zhokey lies at the northern end of the Kazakh Uplands and is part of the Irtysh basin. It lies at an elevation of.

Geographic entities mentioned:
surface_form: zhukey
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 52.89306
lon: 70.58306
For instance, if the road is running through hilly terrain, the carriageways may have to be built on different levels of the slope. An example of this is on the M5 motorway as it climbs up the side of the Gordano Valley south of Bristol. In Birmingham and many other cities, suburban dual carriageways may have trees or cycle lanes in the middle as a wide central reservation.

Geographic entities mentioned:
surface_form: Gordano Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.45315
lon: -2.8145111111111
Planica. Planica () is an Alpine valley in northwestern Slovenia, extending south from the border village of Rateče, not far from another well-known ski resort, Kranjska Gora. Further south, the valley extends into the Tamar Valley, a popular hiking destination in Triglav National Park. Planica is famous for ski jumping.

Geographic entities mentioned:
surface_form: planica
instance_of: Valley
countries: Slovenia
coordinates: lat: 46.476944444444
lon: 13.722222222222
Planica () is an Alpine valley in northwestern Slovenia, extending south from the border village of Rateče, not far from another well-known ski resort, Kranjska Gora. Further south, the valley extends into the Tamar Valley, a popular hiking destination in Triglav National Park. Planica is famous for ski jumping. The first ski jumping hill was constructed before 1930 at the slope of Mount Ponca.

Geographic entities mentioned:
surface_form: planica
instance_of: Valley
countries: Slovenia
coordinates: lat: 46.476944444444
lon: 13.722222222222
The venue was completed in 1934. The first ski jump over in history was achieved at the hill in 1936 by Sepp Bradl. At the time, it was the biggest jumping hill in the world. In 1969, a new K185 hill, the Gorišek Brothers Flying Hill (&quot;Letalnica bratov Gorišek&quot;) was built by Vlado and Janez Gorišek. The FIS Nordic World Ski Championships 2023 were held in Planica.

Geographic entities mentioned:
surface_form: planica
instance_of: Valley
countries: Slovenia
coordinates: lat: 46.476944444444
lon: 13.722222222222
Topock Gorge. Topock Gorge is a mountainous canyon and gorge section of the Colorado River, located between Interstate 40 and Lake Havasu. The town of Needles, California, to the northwest, was named for the &quot;needle-like&quot; vertical rock outcroppings. The natural landmarks and river crossing by them were one of the journey markers for travelers on historic Route 66.

Geographic entities mentioned:
surface_form: topock gorge
instance_of: Lake
countries: United States
coordinates: lat: 34.665263888889
lon: -114.448525
In 1892 he became member of the &quot;Deutsche Akademie der Naturforscher Leopoldina&quot;. He died in Basel. After his death, a donation enabled the construction of the &quot;Zschokke house&quot;, a building located on the Gerschnialp, at the foot of the Titlis, in the ski and hiking resort of Engelberg. Today the structure is used for weekend seminars and workshops.

Geographic entities mentioned:
surface_form: Titlis
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.771944444444
lon: 8.4377777777778
Roughly midway between the two endpoints, NY 8 passes through Utica, where it overlaps NY 5, NY 12, and Interstate 790 (I-790) along one segment of the North–South Arterial. NY 8 was assigned as part of the 1930 renumbering of state highways in New York and originally extended north to a ferry across Lake Champlain at Putnam Station, where it connected to Vermont Route F-10 (VT F-10).

Geographic entities mentioned:
surface_form: Lake Champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
Origins and terminus changes. In the 1930 renumbering of state highways in New York, NY 8 was assigned to most of its current alignment from Deposit to Hague. The route also extended eastward to Wright (southeast of Ticonderoga) on modern NY 9N, NY 22, and County Route 2 (CR 2), where it connected to VT F-10 by way of a ferry across Lake Champlain.

Geographic entities mentioned:
surface_form: Lake Champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
Apis mellifera syriaca. &quot;Apis mellifera syriaca&quot; is known by the common name of the Syrian honey bee, sometimes also called the Palestine honey bee. It occurs from northern Syria, through Lebanon and to Palestine, or southern Israel into the Negev desert and extending past the Jordan Valley into Jordan. It has been claimed that the &quot;A. m.

Geographic entities mentioned:
surface_form: Jordan Valley
instance_of: Valley
countries: Jordan
coordinates: lat: 32.317222
lon: 35.57
Many landmarks in the region were named by him. During these expeditions, Robinson, acting under the policies of the local British colonial government, removed all the Indigenous residents from the area. The far south west was first surveyed from land by James Sprent in 1854 when he reached Port Davey, becoming the first European to notice Federation Peak which he dubbed &quot;the Obelisk&quot;.

Geographic entities mentioned:
surface_form: Federation Peak
instance_of: Mountain
countries: Australia
coordinates: lat: -43.271388888889
lon: 146.47555555556
Alternatively, a flight to or from Melaleuca may be arranged to split the walk, or for tourist access for day trips. Several more difficult walks also exist, encompassing the Eastern and Western Arthur Ranges, Precipitous Bluff, Mount Anne the South West Cape, and Federation Peak. Many of these latter routes are not recommended for inexperienced walkers, or for people traveling alone.

Geographic entities mentioned:
surface_form: Federation Peak
instance_of: Mountain
countries: Australia
coordinates: lat: -43.271388888889
lon: 146.47555555556
Geography. Glyder Fawr is part of the Glyderau mountain range which lies to the northeast of the Snowdon massif, separated from that mountain by the Llanberis Pass and the Nant Peris Valley. Going from west to east, the Glyderau range consists of Elidir Fawr (), Y Garn (), Glyder Fawr (), Glyder Fach () and Tryfan ().

Geographic entities mentioned:
surface_form: Snowdon massif
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.068863888889
lon: -4.0755888888889
surface_form: snowdon
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.068863888889
lon: -4.0755888888889
Geography. Glyder Fawr is part of the Glyderau mountain range which lies to the northeast of the Snowdon massif, separated from that mountain by the Llanberis Pass and the Nant Peris Valley. Going from west to east, the Glyderau range consists of Elidir Fawr (), Y Garn (), Glyder Fawr (), Glyder Fach () and Tryfan ().

Geographic entities mentioned:
surface_form: Elidir Fawr
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.130738888889
lon: -4.0760305555556
surface_form: Glyder Fach
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.10482
lon: -4.00841
surface_form: Tryfan
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.114938888889
lon: -3.9975305555556
surface_form: y garn
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.4505
lon: -3.8031
surface_form: tryfan
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.114938888889
lon: -3.9975305555556
surface_form: y garn
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.115
lon: -4.04837
surface_form: elidir fawr
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.130738888889
lon: -4.0760305555556
surface_form: glyder fawr
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.10147
lon: -4.029164
surface_form: y garn
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.7889
lon: -3.92623
surface_form: glyder fach
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.10482
lon: -4.00841
Going from west to east, the Glyderau range consists of Elidir Fawr (), Y Garn (), Glyder Fawr (), Glyder Fach () and Tryfan (). To the north of the range lie the Carneddau, separated from the Glyderau by the Ogwen Valley and the Nant Ffrancon Valley.

Geographic entities mentioned:
surface_form: Carneddau
instance_of: Landform
countries: United Kingdom
coordinates: lat: 53.18114
lon: -4.00297
surface_form: Nant Ffrancon Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.1484
lon: -4.0414
surface_form: carneddau
instance_of: Landform
countries: United Kingdom
coordinates: lat: 53.18114
lon: -4.00297
surface_form: nant ffrancon
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.1484
lon: -4.0414
surface_form: ogwen valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.125
lon: -4
The ice sheet of the most recent ice age retreated about ten thousand years ago leaving Cwm Idwal as an example of a cirque. The ice scarred the surrounding cliffs, hollowed out the bed of Llyn Idwal and dumped rocks and other material that formed moraines at its foot. Massive boulders and shattered rocks crashed down from above to form the boulder fields and screes visible today.

Geographic entities mentioned:
surface_form: Llyn Idwal
instance_of: Lake
countries: United Kingdom
coordinates: lat: 53.115833333333
lon: -4.0255555555556
surface_form: llyn idwal
instance_of: Lake
countries: United Kingdom
coordinates: lat: 53.115833333333
lon: -4.0255555555556
Routes to the summit. The summit can be accessed from several directions: one route starts at Ogwen Cottage on the shores of Llyn Idwal and approaches the mountain from the north; another starts at Pen-y-Pass and approaches it from the south; another possibility is to approach it from the east along the ridge from Glyder Fach.

Geographic entities mentioned:
surface_form: Llyn Idwal
instance_of: Lake
countries: United Kingdom
coordinates: lat: 53.115833333333
lon: -4.0255555555556
surface_form: llyn idwal
instance_of: Lake
countries: United Kingdom
coordinates: lat: 53.115833333333
lon: -4.0255555555556
surface_form: glyder fach
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.10482
lon: -4.00841
From here a steep scree path ascends the western shoulder to the summit of Glyder Fawr. Management. The National Trust took over the management of the Glyderau and the Carneddau in 1951 in lieu of death duties on the Penrhyn Estate. The total area is about 7,000 hectares, half of which is common land with registered grazing rights for 45,000 sheep and 741 ponies.

Geographic entities mentioned:
surface_form: Carneddau
instance_of: Landform
countries: United Kingdom
coordinates: lat: 53.18114
lon: -4.00297
surface_form: carneddau
instance_of: Landform
countries: United Kingdom
coordinates: lat: 53.18114
lon: -4.00297
A scrambling, circuit route encompasses the three summits of Tryfan, Glyder Fach and Glyder Fawr and takes six or seven hours. One of the most popular routes from Ogwen Cottage follows the shore of Llyn Idwal to the base of the famous Rhiwiau Caws (Idwal Slabs) rock climbing crag, it then makes its way out of the cwm via the steep Twll Du path, arriving at a small lake called Llyn Y Cŵn.

Geographic entities mentioned:
surface_form: llyn idwal
instance_of: Lake
countries: United Kingdom
coordinates: lat: 53.115833333333
lon: -4.0255555555556
Although there is much shattered stone near the summit of Glyder Fach, the ridge between the two summits is fairly level and easy going. A scrambling, circuit route encompasses the three summits of Tryfan, Glyder Fach and Glyder Fawr and takes six or seven hours.

Geographic entities mentioned:
surface_form: tryfan
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.114938888889
lon: -3.9975305555556
surface_form: glyder fawr
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.10147
lon: -4.029164
surface_form: glyder fach
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.10482
lon: -4.00841
Glyder Fawr. Glyder Fawr is a mountain in Snowdonia, Wales, the highest peak in the Glyderau range at just over 1,000 metres. It is the fifth-highest mountain in Wales and has several walking and scrambling routes leading to its summit. According to Sir Ifor Williams, the word &quot; derives from the Welsh word &quot;, meaning a heap of stones. Geography.

Geographic entities mentioned:
surface_form: glyder fawr
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.10147
lon: -4.029164
The Glyderau are separated from the surrounding mountain ranges making them stand out clearly from afar and giving them commanding views of the surrounding peaks and valleys. Until late 2010, most maps showed the height of Glyder Fawr to be; however, the mountain was resurveyed with accurate GPS equipment and its height was found to be.

Geographic entities mentioned:
surface_form: glyder fawr
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.10147
lon: -4.029164
One of the most popular routes from Ogwen Cottage follows the shore of Llyn Idwal to the base of the famous Rhiwiau Caws (Idwal Slabs) rock climbing crag, it then makes its way out of the cwm via the steep Twll Du path, arriving at a small lake called Llyn Y Cŵn. From here a steep scree path ascends the western shoulder to the summit of Glyder Fawr. Management.

Geographic entities mentioned:
surface_form: glyder fawr
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.10147
lon: -4.029164
Although there is much shattered stone near the summit of Glyder Fach, the ridge between the two summits is fairly level and easy going. A scrambling, circuit route encompasses the three summits of Tryfan, Glyder Fach and Glyder Fawr and takes six or seven hours.

Geographic entities mentioned:
surface_form: glyder fach
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.10482
lon: -4.00841
Muskeg Formation. The Muskeg Formation is a geologic formation of Middle Devonian (Givetian) age in the Western Canada Sedimentary Basin. It extends from the plains of northwestern Alberta to northeastern British Columbia, and includes important petroleum and natural gas reservoirs in the Zama lake and Rainbow Lake areas of northwestern Alberta. Lithology.

Geographic entities mentioned:
surface_form: Zama lake
instance_of: Lake
countries: Canada
coordinates: lat: 58.75
lon: -119.08333333333
History. Siuro is one of the original stations of the Tampere–Pori railway, being opened on 4 November 1895. Its location was chosen based on its proximity to the Siuronkoski rapids, as the large lake of Mahnalanselkä – Kirkkojärvi was used as a waterborne route towards Hämeenkyrö. This factor helped Siuro grow into a significant industrial population center in its area.

Geographic entities mentioned:
surface_form: Mahnalanselkä – Kirkkojärvi
instance_of: Lake
countries: Finland
coordinates: lat: 61.58783333
lon: 23.24506667
Historical boundaries. The district was adjacent to the 2nd district to the east and south, the 7th district to the north, and the 3rd and 13th districts to the west, and also bordered the 11th district at its southwest corner. The district's northeast border followed Lake Michigan's shoreline for almost a mile. The district was created following the 1830 U.S.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Blue Harbor Resort. Blue Harbor Resort and Spa is a resort, water park and conference center in Sheboygan, Wisconsin. The resort opened in June 2004 after being built by Great Wolf Resorts. History. Blue Harbor Resort is located on Lake Michigan at the mouth of the Sheboygan River on the C. Reiss Coal Peninsula. The peninsula had formerly been used for coal storage.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Drielaker See. The Drielaker See is a coastal lake in Osternburg subdistrict of Drielake in the municipal area of Oldenburg, Niedersachsen. Description. The 10.4 ha lake was created during the construction of the Autobahn A 29 in the 1980s. The reason for this evacuation was for the construction of the ramps for the 26 meter high motorway viaduct.

Geographic entities mentioned:
surface_form: drielaker see
instance_of: Lake
countries: Germany
coordinates: lat: 53.13471
lon: 8.252341944444444
Today it is used a recreational area with close proximity to the port and commercial areas. The Drielaker See is used by the Sport Fishing Club of Oldenburg (Sportfischer-Verein Oldenburg e.V.) for angling. The Hemmelsbäker Canal runs directly from the northeastern side of the lake, which leads into the Hunte about 100 meters further north.

Geographic entities mentioned:
surface_form: drielaker see
instance_of: Lake
countries: Germany
coordinates: lat: 53.13471
lon: 8.252341944444444
It is situated about to the west of Morpeth. The population at the 2011 census was 194. The place-name 'Hartburn' is first attested in Charter Rolls of 1198, where it appears as &quot;Herteburne&quot;. The name means 'stag stream'. The village is on the Hart Burn river, which a couple of miles downstream joins the River Wansbeck, which flows through Morpeth and Ashington to the sea. Landmarks.

Geographic entities mentioned:
surface_form: Hart Burn
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 55.159668
lon: -1.830864
Habitat and distribution. Rainforests, mature secondary woodland forests and forest edges are typical habitats in which Philippine scops owls can be found. They are mostly observed in the understory and rarely go above 1,000 m altitudes, with the exception of individuals which were reported on Mount Data, Luzon.

Geographic entities mentioned:
surface_form: Mount Data
instance_of: Mountain
countries: Philippines
coordinates: lat: 16.8833
lon: 120.8466
In 1886, he was made general superintendent of the western division, with headquarters at Winnipeg, and in 1896 was advanced to the position of general manager of all lines and branches from Lake Superior to the Pacific coast. In 1901, he became an assistant to the president and was made second vice president in 1904. In 1910, he became vice president until his resignation in 1911.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
Lake Terrace/Lake Oaks, New Orleans. Lake Terrace/Lake Oaks is a neighborhood of the city of New Orleans, Louisiana. A sub-district of the city's Gentilly District, its boundaries as defined by the City Planning Commission are: Lake Pontchartrain to the north; the Industrial Canal to the east; Leon C.

Geographic entities mentioned:
surface_form: Lake Pontchartrain
instance_of: Lake
countries: United States
coordinates: lat: 30.188888888889
lon: -90.101388888889
It is considered one of the wealthier areas of the city. History. This was the original location of Milneburg, whose historic name has been revived by a modern neighborhood somewhat farther south. Land was reclaimed from Lake Pontchartrain in an Orleans Levee Board project which began in the 1920s and was completed in the 1930s, creating the space now occupied by the neighborhood.

Geographic entities mentioned:
surface_form: Lake Pontchartrain
instance_of: Lake
countries: United States
coordinates: lat: 30.188888888889
lon: -90.101388888889
Bagmasti. 7h18eaw06nn7wagumyfpzymkdxfk" xml:space="preserve">Bagmasti () was a famous Armenian goddess. She was worshiped at Musasir in Ararat and was the companion or consort of Ḫaldi. Her temple, together with that of Ḫaldi was plundered and burned by Sargon II king of Assyria.

Geographic entities mentioned:
surface_form: Ararat
instance_of: Mountain
countries: Turkey
coordinates: lat: 39.70194444444444
lon: 44.29833333333333
Today, the Cheshire Mills are protected as part of the Harrisville Historic District, a National Historic Landmark which includes the center of town. With its red brick buildings and mills reflected in Harrisville Pond and canal, the village is frequently photographed as an iconic example of picturesque old New England.

Geographic entities mentioned:
surface_form: Harrisville Pond
instance_of: Lake
countries: United States
coordinates: lat: 42.9456
lon: -72.0961
Significant water bodies include Silver Lake, Seaver Reservoir, and Chesham Pond on the western side, and Harrisville Pond and Skatutakee Lake draining to the east. Churches. The Community Church of Harrisville and Chesham was formed from Chesham Baptist Church and Harrisville Congregational Church. Chesham Baptist Church dates back to 1785.

Geographic entities mentioned:
surface_form: Harrisville Pond
instance_of: Lake
countries: United States
coordinates: lat: 42.9456
lon: -72.0961
surface_form: Skatutakee Lake
instance_of: Lake
countries: United States
coordinates: lat: 42.937777777778
lon: -72.074444444444
He also served on an ATF Special Response Team, a federal equivalent of a SWAT team. In early 1998, as part of an operation to infiltrate motorcycle gangs, Queen joined the San Fernando Valley chapter of the Mongols Motorcycle Club as &quot;Billy St. John&quot;, and was a member for 28 months.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
Qezel Arsalan. Qezel Arsalan, (also Ghezel Arsala) (Azerbaijani language: Qızıl Ərsalan, Persian language:قزل ارسلان) is a mountain peak with a height of 3,250 meters in the Alvand ranges of the Zagros mountains in western Iran. An Iranian movie of the same name was produced in 1956.

Geographic entities mentioned:
surface_form: Alvand
instance_of: Mountain
countries: Iran
coordinates: lat: 34.664166666667
lon: 48.486666666667
surface_form: قزل ارسلان
instance_of: Mountain
countries: Iran
coordinates: lat: 34.75821889
lon: 48.33186167
surface_form: qezel arsalan
instance_of: Mountain
countries: Iran
coordinates: lat: 34.75821889
lon: 48.33186167
Qezel Arsalan. Qezel Arsalan, (also Ghezel Arsala) (Azerbaijani language: Qızıl Ərsalan, Persian language:قزل ارسلان) is a mountain peak with a height of 3,250 meters in the Alvand ranges of the Zagros mountains in western Iran. An Iranian movie of the same name was produced in 1956.

Geographic entities mentioned:
surface_form: qezel arsalan
instance_of: Mountain
countries: Iran
coordinates: lat: 34.75821889
lon: 48.33186167
Steele was ordained in the Anglican Diocese of Sydney where he is a member of the diocese's synod, standing committee, mission board and the South Sydney Regional Council. Steele was appointed as lay minister in charge of St Aidan's Anglican Church in Annandale in 2002. He was ordained in 2003 and remained in charge of St Aidan's.

Geographic entities mentioned:
surface_form: Annandale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 55.2
lon: -3.4
Clayton Falls Creek. Clayton Falls Creek is a creek in the Central Coast of British Columbia. It flows through a forested river valley into the North Bentinck Arm about east of the community of Bella Coola. The Clayton Falls Dam, a small concrete gravity dam, is located on the river.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: clayton falls creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 52.37036
lon: -126.81583
Clayton Falls Creek is a creek in the Central Coast of British Columbia. It flows through a forested river valley into the North Bentinck Arm about east of the community of Bella Coola. The Clayton Falls Dam, a small concrete gravity dam, is located on the river. Although managed by BC Hydro, it is the only dam in British Columbia not integrated into the agency's integrated hydroelectric system.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
History. The river is within the traditional territory of the Nuxalk people. Around 1935, the British Columbia Water Rights Branch named the creek after John Clayton, an early settler of the region and a factor (agent) of the Hudson's Bay Company. This name was given as &quot;Clayton Creek&quot; in the 1930 BC Gazetteer, but the name Clayton Falls Creek was officially adopted in 1953.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
Clayton Falls Creek. Clayton Falls Creek is a creek in the Central Coast of British Columbia. It flows through a forested river valley into the North Bentinck Arm about east of the community of Bella Coola. The Clayton Falls Dam, a small concrete gravity dam, is located on the river.

Geographic entities mentioned:
surface_form: clayton falls creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 52.37036
lon: -126.81583
Clearcut logging devastated the watershed in 1991; the forestland in the basin is now divided into two protected areas — the Clayton Falls Conservancy and the Bella Coola Community Forest. Geography and hydrology. Clayton Falls Creek has its headwaters near Mount Fougner in the Pacific Ranges. It flows through a river valley until it reaches its highest falls and the nearby Clayton Falls Dam.

Geographic entities mentioned:
surface_form: clayton falls creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 52.37036
lon: -126.81583
Flow rates are generally lowest in the winter, although this is disrupted by the occasional outbreak of heavy rain, where the creek sees its peak flow. Watershed. The Clayton Falls Creek watershed is around in area. Almost the entirety of the watershed is crown land.

Geographic entities mentioned:
surface_form: clayton falls creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 52.37036
lon: -126.81583