Sarmila/GeoWiki-Features huggingface dataset:
In terms of the area, Lake Vozhe is the third natural lake of Vologda Oblast (behind Lake Onega and Lake Beloye and just ahead of Lake Kubenskoye) and the fourth lake (also behind the Rybinsk Reservoir). Historically, Lake Vozhe was on the trading route connecting the basings of the Volga and the Onega via the Sheksna. There is one big island on the lake, Spassky Island.

Geographic entities mentioned:
surface_form: onega
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 61.690555555556
lon: 35.655555555556
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
surface_form: lake vozhe
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 60.589444444444
lon: 39.0925
surface_form: vozhe
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 60.589444444444
lon: 39.0925
Lake Vozhe. Lake Vozhe, also known as Lake Charondskoye (), is a lake in the northern part of Vologda Oblast in Russia. The area of the lake is, and the area of its basin is. The average depth is around (maximum depth is). Lake Vozhe drains through the Svid into Lake Lacha, from which the Onega flows out. The lake is located on a flatland and its shores are low-lying and swampy.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
surface_form: lake vozhe
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 60.589444444444
lon: 39.0925
surface_form: vozhe
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 60.589444444444
lon: 39.0925
Lake Vozhe. Lake Vozhe, also known as Lake Charondskoye (), is a lake in the northern part of Vologda Oblast in Russia. The area of the lake is, and the area of its basin is. The average depth is around (maximum depth is). Lake Vozhe drains through the Svid into Lake Lacha, from which the Onega flows out. The lake is located on a flatland and its shores are low-lying and swampy.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
surface_form: lake vozhe
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 60.589444444444
lon: 39.0925
surface_form: vozhe
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 60.589444444444
lon: 39.0925
Lake Vozhe. Lake Vozhe, also known as Lake Charondskoye (), is a lake in the northern part of Vologda Oblast in Russia. The area of the lake is, and the area of its basin is. The average depth is around (maximum depth is). Lake Vozhe drains through the Svid into Lake Lacha, from which the Onega flows out. The lake is located on a flatland and its shores are low-lying and swampy.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
The average depth is around (maximum depth is). Lake Vozhe drains through the Svid into Lake Lacha, from which the Onega flows out. The lake is located on a flatland and its shores are low-lying and swampy. The biggest swamp, the Charonda Swamp, is located to the southeast of the lake. Around twenty rivers flow into Lake Vozhe, including the Vozhega and the Modlona.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
The lake is located on a flatland and its shores are low-lying and swampy. The biggest swamp, the Charonda Swamp, is located to the southeast of the lake. Around twenty rivers flow into Lake Vozhe, including the Vozhega and the Modlona. The lake freezes up in October - November (some parts freeze to the very bottom) and stays icebound until May.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
surface_form: lake vozhe
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 60.589444444444
lon: 39.0925
surface_form: vozhe
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 60.589444444444
lon: 39.0925
The biggest swamp, the Charonda Swamp, is located to the southeast of the lake. Around twenty rivers flow into Lake Vozhe, including the Vozhega and the Modlona. The lake freezes up in October - November (some parts freeze to the very bottom) and stays icebound until May. Administratively, the lake is divided between Kirillovsky District (west) and Vozhegodsky District (east) of Vologda Oblast.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
Administratively, the lake is divided between Kirillovsky District (west) and Vozhegodsky District (east) of Vologda Oblast. The northern shore belongs to Kargopolsky and Konoshsky District of Arkhangelsk Oblast, but the boundary between the oblasts is drawn such that the whole area of the lake is in Vologda Oblast.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
Historically, Lake Vozhe was on the trading route connecting the basings of the Volga and the Onega via the Sheksna. There is one big island on the lake, Spassky Island. On the island, ruins of the former monastery are located.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
Charonda does not have all-seasonal land connections. Formerly, the village of Vasilyevskaya was located on the northern lakeshore. It had a railway station, Svid station, on the railway connecting the settlement of Yertsevo and the village of Sovza, located west of the lake. In Sovza, a number of prison camps were operating, and the railroad was used to transport timber.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
Warden of the Marches. In December 1559 Grey was constituted governor of Berwick, warden of the middle marches towards Scotland, and warden of Tynedale and Redesdale. He went down to the border with two thousand men nominally to reinforce the Berwick garrison, but at first with a large latitude of action.

Geographic entities mentioned:
surface_form: Redesdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 55.229
lon: -2.186
Smoothrock Lake. Smoothrock Lake is a lake in the Unorganized Part of Thunder Bay District in Northern Ontario, Canada. It is in the James Bay drainage basin and lies in Wabakimi Provincial Park. The lake has three major inflows: the Caribou River at Caribou Bay at the east; and the Boiling Sand River and the Lookout River, at the south. A secondary inflow is Berry Creek at the southwest.

Geographic entities mentioned:
surface_form: sand river
instance_of: Watercourse
countries: Canada
coordinates: lat: 45.532222222222224
lon: -64.67861111111111
A secondary inflow is Berry Creek at the southwest. The main outflow is the Berg River from Outlet Bay at the north centre, and leads north to the Ogoki River. A secondary outflow, unnamed and at the northeast, heads from Lonebreast Bay north through a series of lakes to Whitewater Lake, further downstream on the Ogoki River. The Ogoki River flows via the Albany River to James Bay.

Geographic entities mentioned:
surface_form: whitewater lake
instance_of: Lake
countries: Canada
coordinates: lat: 46.53333333333333
lon: -81.14166666666667
surface_form: whitewater lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.23805556
lon: -100.32361111
Smoothrock Lake. Smoothrock Lake is a lake in the Unorganized Part of Thunder Bay District in Northern Ontario, Canada. It is in the James Bay drainage basin and lies in Wabakimi Provincial Park. The lake has three major inflows: the Caribou River at Caribou Bay at the east; and the Boiling Sand River and the Lookout River, at the south. A secondary inflow is Berry Creek at the southwest.

Geographic entities mentioned:
surface_form: smoothrock lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.542
lon: -89.436
Gen. George P. Doles was killed. Cook was wounded again at the Battle of the Crater during the Siege of Petersburg. After recovering, he fought under Maj. Gen. Stephen D. Ramseur at the Battle of Cedar Creek in the Shenandoah Valley before returning with his men to the trenches around Petersburg, Virginia. He was wounded a third time during the 1865 attack on Fort Stedman.

Geographic entities mentioned:
surface_form: Shenandoah Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.5
lon: -78.85
Scituate is considered a South Shore community, located just south of the mouth of greater Boston Harbor. The town is not contiguous; Humarock is a part of Scituate which can only be reached from Marshfield. The latter was formerly connected to the town, but that connection was lost when the mouth of the South River shifted northward as the result of the Portland Gale of 1898.

Geographic entities mentioned:
surface_form: Humarock
instance_of: Landform
countries: United States
coordinates: lat: 42.1361
lon: -70.6906
In the early Bronze Age, the region was probably inhabited only relatively sparsely, as few noble metals occur here and the soils are only moderately fertile. However, in the late Bronze Age, a warrior elite of the so-called Urnfield culture (1200-800 BC) began to establish themselves on hilltops like the Ehrenbürg, the Hesselberg or the Marienberg above Würzburg.

Geographic entities mentioned:
surface_form: Ehrenbürg
instance_of: Mountain
countries: Germany
coordinates: lat: 49.713888888889
lon: 11.1575
surface_form: Hesselberg
instance_of: Mountain
countries: Germany
coordinates: lat: 49.07
lon: 10.526944444444
They built a chain of hillforts in northern Franconia as a defensive line against the Germani who were pressing in from the north. On the Staffelberg they built a mighty settlement, which was mentioned by Ptolemy under the name of &quot;oppidum Menosgada&quot;. Another was built on the Gleichberge: the largest surviving oppidum in Central Germany, the Steinsburg.

Geographic entities mentioned:
surface_form: Staffelberg
instance_of: Mountain
countries: Germany
coordinates: lat: 50.092222222222
lon: 11.024722222222
This defensive line bisected the south of Franconia and describes an arc through the region whose northernmost point was located at today's Gunzenhausen. To oversee it, the Romans built several forts, such as Biriciana near Weißenburg or Ruffenhofen at the foot of the Hesselberg.

Geographic entities mentioned:
surface_form: Hesselberg
instance_of: Mountain
countries: Germany
coordinates: lat: 49.07
lon: 10.526944444444
Fortified settlements as on the Gelbe Bürg near Dittenheim and Reisberg at Scheßlitz controlled the new regions. But north of the former &quot;Limes&quot;, for example on the Ehrenbürg, the Staffelberg or the Houbirg, more such &quot;Gau castles&quot; (&quot;Gauburgen&quot;) have been detected. What tribe their occupants belonged to is unknown in most cases.

Geographic entities mentioned:
surface_form: Ehrenbürg
instance_of: Mountain
countries: Germany
coordinates: lat: 49.713888888889
lon: 11.1575
Occurrence. Kesterite was first described in 1958 in regard to an occurrence in the Kester deposit (and the associated locality) in Ynnakh Mountain, Yana basin, Yakutia, Russia, where it was discovered. It is usually found in quartz-sulfide hydrothermal veins associated with tin ore deposits.

Geographic entities mentioned:
surface_form: Ynnakh Mountain
instance_of: Mountain
countries: Russia
Soviet Union
Russian Empire
coordinates: lat: 67.41666666666667
lon: 134.86666666666667
The valley then splits, one branch following the Dawa River west along the Ethiopia-Kenya frontier, then north into Ethiopia, and the other branch follows the Ganale Dorya River north into Ethiopia. Along with the Shebelle Valley, and the nearby Chamo and Abaya lakes, the Jubba Valley is considered an Endemic Bird Area by Birdlife International.

Geographic entities mentioned:
surface_form: Shebelle Valley
instance_of: Valley
countries: Ethiopia
Somalia
coordinates: lat: 4.7333333333333
lon: 45.2
surface_form: Chamo
instance_of: Lake
countries: Ethiopia
coordinates: lat: 5.8333333333333
lon: 37.55
surface_form: Abaya
instance_of: Lake
countries: Ethiopia
coordinates: lat: 6.236
lon: 37.832
surface_form: jubba valley
instance_of: Valley
countries: Ethiopia
Somalia
Kenya
coordinates: lat: 4.1772222222222
lon: 42.079444444444
Jubba Valley. The Jubba Valley () is a valley in East Africa. It follows the line of the Jubba River north from the Indian Ocean to the Somalia-Ethiopia border. The valley then splits, one branch following the Dawa River west along the Ethiopia-Kenya frontier, then north into Ethiopia, and the other branch follows the Ganale Dorya River north into Ethiopia.

Geographic entities mentioned:
surface_form: jubba valley
instance_of: Valley
countries: Ethiopia
Somalia
Kenya
coordinates: lat: 4.1772222222222
lon: 42.079444444444
Along with the Shebelle Valley, and the nearby Chamo and Abaya lakes, the Jubba Valley is considered an Endemic Bird Area by Birdlife International. The Somali section of Jubba Valley is known as Jubaland.

Geographic entities mentioned:
surface_form: jubba valley
instance_of: Valley
countries: Ethiopia
Somalia
Kenya
coordinates: lat: 4.1772222222222
lon: 42.079444444444
In 2019 the British ambassador to the Czech Republic, Nick Archer, unveiled a plaque on the building in the Letná area of Prague in which the early seminars were held. Background. The Foundation was created after Czech dissident philosopher Julius Tomin wrote in 1978 to four Western universities asking them to support philosophy seminars he was holding in his apartment in Prague.

Geographic entities mentioned:
surface_form: Letná
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.0957
lon: 14.4165
Rosställispitz. The Rosställispitz is a mountain of the Silvretta Alps, located west of Susch in the canton of Graubünden. It lies between the valleys of Vereina and Fless, north-east of the Flüela Wisshorn.

Geographic entities mentioned:
surface_form: Flüela Wisshorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.76212
lon: 9.96661
Rosställispitz. The Rosställispitz is a mountain of the Silvretta Alps, located west of Susch in the canton of Graubünden. It lies between the valleys of Vereina and Fless, north-east of the Flüela Wisshorn.

Geographic entities mentioned:
surface_form: rosställispitz
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.78888889
lon: 9.99333333
In Richtersveld. Shankar, highly inspired by Alvarez's exploits, resigns from his job and accompanies Alvarez as they decide to venture out once more and find the mines. They meet with innumerable hardships, and come across the raging volcano called Ol Doinyo Lengai. But the volcano was uncharted by the world outside, thus making Shankar and Alvarez its first discoverers.

Geographic entities mentioned:
surface_form: Ol Doinyo Lengai
instance_of: Mountain
countries: Tanzania
coordinates: lat: -2.7616666666667
lon: 35.913333333333
Eventually, they get lost in the forests where Alvarez suffers death at the hands of a mysterious monster, the same that had taken Carter’s life, the Bunyip. Legacy. After returning from the &quot;Mountain of the Moon&quot; Shankar wrote an article for a local newspaper where he refers to the Ol Doinyo Lengai volcano as &quot;Mount. Alvarez&quot;. Film.

Geographic entities mentioned:
surface_form: Ol Doinyo Lengai
instance_of: Mountain
countries: Tanzania
coordinates: lat: -2.7616666666667
lon: 35.913333333333
Patscher Spitze. The Patscher Spitze is a mountain of the Rieserferner group on the border between Tyrol, Austria, and South Tyrol, Italy.

Geographic entities mentioned:
surface_form: patscher spitze
instance_of: Mountain
countries: Austria
Italy
coordinates: lat: 46.924166666667
lon: 12.158055555556
This family is known for its many important Jewish Sages over the course of several generations. Some tannaim are considered to belong to this family; the best known of these is Judah ben Bathyra, who resided in Nusaybin west to Babylon. According to Heinrich Graetz, the family is named after the city Batira (בטירא), near Mount Hermon, which was settled by Herod and gave its name to the settlers.

Geographic entities mentioned:
surface_form: Mount Hermon
instance_of: Mountain
countries: Lebanon
Israel
Syria
coordinates: lat: 33.4
lon: 35.85
At the 2021 Census, the population of its urban area was 264,349. The River Great Ouse forms the northern boundary of the urban area; a tributary, the River Ouzel, meanders through its linear parks and balancing lakes. Approximately 25% of the urban area is parkland or woodland and includes two Sites of Special Scientific Interest (SSSIs). The city is made up of many different districts.

Geographic entities mentioned:
surface_form: River Ouzel
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 51.882222222222
lon: -0.63555555555556
The nearest larger towns are Northampton, Bedford, Luton and Aylesbury. The nearest larger cities are Coventry, Leicester, Cambridge, London and Oxford. Geology. Its highest points are in the centre () and at Woodhill on the western boundary (). The lowest point of the urban area is in Newport Pagnell, where the Ouzel joins the Great Ouse (). Parks and environmental infrastructure.

Geographic entities mentioned:
surface_form: Ouzel
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 51.882222222222
lon: -0.63555555555556
Parks and environmental infrastructure. Because of the (poorly drained) clay soils and the urban hard surfaces, the development corporation identified water runoff into the Ouzel and its tributaries as a significant risk to be managed and so put in place two large balancing lakes (Caldecotte and Willen) and a number of smaller detention ponds.

Geographic entities mentioned:
surface_form: Willen
instance_of: Lake
countries: United Kingdom
coordinates: lat: 52.05101
lon: -0.71832
These provide an important leisure amenity for most of the year. Building in the floodplains of the Ouse and Ouzel was precluded too, thus providing long-distance linear parks that are within easy reach of most residents. The north basin of Willen Lake is a bird sanctuary, with a Peace Pagoda and Buddhist temple by the lake.

Geographic entities mentioned:
surface_form: Willen Lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 52.05101
lon: -0.71832
As of 2014, local plans have protected the existing boulevard framework and set higher standards for architectural excellence. Linear parks. The flood plains of the Great Ouse and of its tributaries (the Ouzel and some brooks) have been protected as linear parks that run right through Milton Keynes; these were identified as important landscape and flood-management assets from the outset.

Geographic entities mentioned:
surface_form: Ouzel
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 51.882222222222
lon: -0.63555555555556
The small parish church (1680) at Willen was designed by the architect and physicist Robert Hooke. Nearby, by Willen Lake, there is a Buddhist Temple and the Peace Pagoda, which was built in 1980 and was the first built by the Nipponzan-Myōhōji Buddhist Order in the western world. The original Wolverton was a medieval settlement just north and west of today's town.

Geographic entities mentioned:
surface_form: Willen Lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 52.05101
lon: -0.71832
Many other sports are represented at amateur level. Near the central station, in a space beside the former Milton Keynes central bus station, there is a purpose-built street skateboarding plaza named the Buszy. Willen Lake hosts watersports on the south basin. New technologies. In recent years, the City Council has promoted MK as a test-bed for experimental urban technologies.

Geographic entities mentioned:
surface_form: Willen Lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 52.05101
lon: -0.71832
At the 2021 census the community had a population of 3,485, making it the second-smallest city in the United Kingdom in terms of population. It was historically in Flintshire. The city of St Asaph is surrounded by countryside and views of the Vale of Clwyd. It is situated close to a number of towns including Denbigh, Rhuddlan, Rhyl, Holywell and Abergele. History.

Geographic entities mentioned:
surface_form: Vale of Clwyd
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.21
lon: -3.38
Lavangsdalen. Lavangsdalen () is a valley in Troms, Norway. It runs from Lavangen at Balsfjorden in Balsfjord Municipality northwards to Sørbotn in the end of Ramfjorden in Tromsø Municipality. The valley is mainly known for its stretch of the European route E8, a road branching off from the E6 at Nordkjosbotn to Tromsø.

Geographic entities mentioned:
surface_form: lavangsdalen
instance_of: Valley
countries: Norway
coordinates: lat: 69.44174
lon: 19.2433
Three men were indicted in Nord-Troms District Court; two who were accused of causing the initial crash, as well as the driver who later hit the responders. The last was acquitted, whereas the first two were given short prison sentences. Shortly after the 2008 trial, a landslide blocked the entire Lavangsdalen valley. The landslide was about 80 metres wide.

Geographic entities mentioned:
surface_form: lavangsdalen
instance_of: Valley
countries: Norway
coordinates: lat: 69.44174
lon: 19.2433
This time, the road was highly slippery. She was the driver of a small car that turned 180 degrees, swerved into the opposite lane and hit a trailer truck. With the backside of her car being crushed, she initially survived the accident before succumbing later the same day. Drivers in the area criticized the snow plowing in Lavangsdalen at the time for being inadequate.

Geographic entities mentioned:
surface_form: lavangsdalen
instance_of: Valley
countries: Norway
coordinates: lat: 69.44174
lon: 19.2433
Based on the car's mowing down of the trees, police suspected excessive speed. The driver was pronounced dead on arrival. The Norwegian National Road Policing Service stated that they patrolled Lavangsdalen some time during the day, every single day. Despite being fairly short, European route E8 in Troms had become the most accident-prone in Northern Norway alongside National Road 80.

Geographic entities mentioned:
surface_form: lavangsdalen
instance_of: Valley
countries: Norway
coordinates: lat: 69.44174
lon: 19.2433
Despite being fairly short, European route E8 in Troms had become the most accident-prone in Northern Norway alongside National Road 80. From 2000 to 2010, 17 people died in 10 accidents; of these, 4 accidents with 6 fatalities took place in Lavangsdalen. The death toll would rise drastically in 2011. 2011 accident and aftermath.

Geographic entities mentioned:
surface_form: lavangsdalen
instance_of: Valley
countries: Norway
coordinates: lat: 69.44174
lon: 19.2433
The death toll would rise drastically in 2011. 2011 accident and aftermath. The Lavangsdalen bus accident () was a bus crash in northern Norway on 7 January 2011. On the European route E8, a car headed north towards Tromsø was about to pass a bus headed south towards Nordkjosbotn, but entered the opposing lane and crashed into the bus.

Geographic entities mentioned:
surface_form: lavangsdalen
instance_of: Valley
countries: Norway
coordinates: lat: 69.44174
lon: 19.2433
Yet another person died in July 2011, when a driver crashed through the guard rail, stopping in the adjacent trees. In February 2011, Minister of Transport Magnhild Meltveit Kleppa vowed to install a median barrier in Lavangsdalen. The first monetary allocation came in the fall of 2011, and the pre-project was fully financed by May 2012. The total cost was stipulated at.

Geographic entities mentioned:
surface_form: lavangsdalen
instance_of: Valley
countries: Norway
coordinates: lat: 69.44174
lon: 19.2433
With the Solberg's Cabinet being a minority government, they usually relied on support from the Progress Party, but the Progress Party representative, Per-Willy Amundsen, gave an ultimatum to vote down the National Transport Plan if the plan did not include more medians in Lavangsdalen.

Geographic entities mentioned:
surface_form: lavangsdalen
instance_of: Valley
countries: Norway
coordinates: lat: 69.44174
lon: 19.2433
The collection was compiled in the 18th century by Nicodemus the Hagiorite and Macarius of Corinth based on the codices 472 (12th century), 605 (13th century), 476 (14th century), 628 (14th century) and 629 (15th century) from the library of the monastery of Vatopedi, Mount Athos.

Geographic entities mentioned:
surface_form: Mount Athos
instance_of: Mountain
countries: Greece
coordinates: lat: 40.15833333333333
lon: 24.327222222222222
History. Nikodemos and Makarios were monks at Mount Athos, a mountainous peninsula in northern Greece, historically considered the geographical center of Orthodox spirituality and home to 20 monasteries. The first edition, in Greek, was published in Venice in 1782, with a second Greek edition published in Athens in 1893.

Geographic entities mentioned:
surface_form: Mount Athos
instance_of: Mountain
countries: Greece
coordinates: lat: 40.15833333333333
lon: 24.327222222222222
Gradac (river). The Gradac (, Gradac,) is a river in western Serbia, a tributary of the Kolubara. It cuts a canyon in south–north direction with a length of 22.7 km. Its measured water course has a length of about 28 km and a total drop of 187 m. The source of the river Gradac is situated at the foot of the Povlen mountain. Description.

Geographic entities mentioned:
surface_form: Povlen
instance_of: Mountain
countries: Serbia
coordinates: lat: 44.132777777778
lon: 19.748888888889
Sheldon, the chairman of the influential Boone and Crockett Club, successfully campaigned with Congress to have the area set aside as a national park. In 1917, Denali National Park was established as Mount McKinley National Park. Denali expedition. On March 27, 1912, Hudson Stuck, Episcopal Archdeacon of the Yukon, sent Karstens a letter inviting him to join an expedition to climb Denali.

Geographic entities mentioned:
surface_form: Denali
instance_of: Mountain
countries: United States
coordinates: lat: 63.06916666666667
lon: -151.0063888888889
Juanita Beach Park. Juanita Beach Park is a waterfront park located on the northeast shore of Lake Washington in the Juanita neighborhood, managed by the city of Kirkland, Washington in the United States. It was historically the home of several popular private beach resorts before their purchase by the public in 1956.

Geographic entities mentioned:
surface_form: Lake Washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
As a result of the 1916 construction of the Lake Washington Ship Canal, the lake dropped to match Lake Union's level, which exposed a white sand beach along what is now Juanita Beach. This, as well as the bay's naturally long shelf, which creates a shallow expanse of water out to, made the site a fit for recreation.

Geographic entities mentioned:
surface_form: Lake Union
instance_of: Lake
countries: United States
coordinates: lat: 47.6392
lon: -122.3337
Eighteen years later, in 1940, the dam was rebuilt by the Bureau of Reclamation. The reservoir now serves as one of Oregon's largest rainbow trout fisheries. The heaviest fish ever caught in the lake was a trout. The Deschutes River, which originates at Little Lava Lake, flows south for to Crane Prairie Reservoir. The river leaves the reservoir via the dam and continues south to Wickiup Reservoir.

Geographic entities mentioned:
surface_form: Little Lava Lake
instance_of: Lake
countries: United States
coordinates: lat: 43.910394444444
lon: -121.75669722222
Bay Lake (Minnesota). Bay Lake is a body of water located in the Brainerd Lakes region of Minnesota. The lake has a surface area of and approximately of shoreline. The maximum depth of the lake is with a water clarity of.

Geographic entities mentioned:
surface_form: bay lake
instance_of: Lake
countries: United States
coordinates: lat: 28.416111111111
lon: -81.567777777778
surface_form: bay lake
instance_of: Lake
countries: United States
coordinates: lat: 46.3854
lon: -93.8565
The maximum depth of the lake is with a water clarity of. The Ojibway called the lake Ses-sa-beg-a-mah, which has been translated as &quot;lake of many bays&quot; or &quot;lake of many arms.&quot;
Bay Lake is located within Bay Lake Township, approximately east of Brainerd, Minnesota and five miles (8 km) northwest of Garrison, Minnesota.

Geographic entities mentioned:
surface_form: bay lake
instance_of: Lake
countries: United States
coordinates: lat: 28.416111111111
lon: -81.567777777778
surface_form: bay lake
instance_of: Lake
countries: United States
coordinates: lat: 28.416111111111
lon: -81.567777777778
surface_form: bay lake
instance_of: Lake
countries: United States
coordinates: lat: 46.3854
lon: -93.8565
surface_form: bay lake
instance_of: Lake
countries: United States
coordinates: lat: 46.3854
lon: -93.8565
Like many other lakes in the area, Bay Lake is surrounded by commercial resorts and private cabins, and is a popular destination for fishing, boating, and water skiing. Access to the lake and resorts is via Minnesota State Highway 6 for the western shore and Crow Wing County Highway 10 for the eastern shore. There are three islands on the lake.

Geographic entities mentioned:
surface_form: bay lake
instance_of: Lake
countries: United States
coordinates: lat: 28.416111111111
lon: -81.567777777778
surface_form: bay lake
instance_of: Lake
countries: United States
coordinates: lat: 46.3854
lon: -93.8565
Geikie Peak. Geikie Peak is a -elevation summit located in the Grand Canyon, in Coconino County of northern Arizona, United States. It is situated northwest of Grand Canyon Village, immediately north of Diana Temple, and south of Scorpion Ridge which lies across the opposite side of Granite Gorge. Access is via the Tonto Trail which traverses 270 degrees around the base of the peak.

Geographic entities mentioned:
surface_form: grand canyon
instance_of: Valley
countries: United States
coordinates: lat: 38.65888889
lon: -91.10388889
surface_form: geikie peak
instance_of: Mountain
countries: United States
coordinates: lat: 36.13304
lon: -112.26962
Geikie Peak. Geikie Peak is a -elevation summit located in the Grand Canyon, in Coconino County of northern Arizona, United States. It is situated northwest of Grand Canyon Village, immediately north of Diana Temple, and south of Scorpion Ridge which lies across the opposite side of Granite Gorge. Access is via the Tonto Trail which traverses 270 degrees around the base of the peak.

Geographic entities mentioned:
surface_form: grand canyon
instance_of: Valley
countries: United States
coordinates: lat: 38.65888889
lon: -91.10388889
surface_form: diana temple
instance_of: Landform
countries: United States
coordinates: lat: 36.1119
lon: -112.2738
History. George Wharton James named it &quot;Geikie Monument&quot; in 1901 for Sir Archibald Geikie (1835–1924), Director General of the Geological Survey of the United Kingdom, who studied geology in the Grand Canyon, finding evidence to support his theories of erosion. This feature's present name was officially adopted in 1908 by the U.S. Board on Geographic Names. Geology.

Geographic entities mentioned:
surface_form: grand canyon
instance_of: Valley
countries: United States
coordinates: lat: 38.65888889
lon: -91.10388889
Scylla Butte. At the end of Geikie Peak's east spur lies a smaller feature called Scylla Butte. This feature is named for Scylla, a monster according to Greek mythology, in keeping with Clarence Dutton's practice of naming geographical features in the Grand Canyon after mythological deities. It rises approximately 400 feet above the Tonto Trail which nearly surrounds it.

Geographic entities mentioned:
surface_form: grand canyon
instance_of: Valley
countries: United States
coordinates: lat: 38.65888889
lon: -91.10388889
surface_form: scylla
instance_of: Mountain
countries: United States
coordinates: lat: 37.07994
lon: -118.68955
surface_form: dutton
instance_of: Mountain
countries: United States
coordinates: lat: 55.168
lon: -162.272
Scylla Butte. At the end of Geikie Peak's east spur lies a smaller feature called Scylla Butte. This feature is named for Scylla, a monster according to Greek mythology, in keeping with Clarence Dutton's practice of naming geographical features in the Grand Canyon after mythological deities. It rises approximately 400 feet above the Tonto Trail which nearly surrounds it.

Geographic entities mentioned:
surface_form: scylla
instance_of: Mountain
countries: United States
coordinates: lat: 37.07994
lon: -118.68955
surface_form: geikie peak
instance_of: Mountain
countries: United States
coordinates: lat: 36.13304
lon: -112.26962
Geikie Peak. Geikie Peak is a -elevation summit located in the Grand Canyon, in Coconino County of northern Arizona, United States. It is situated northwest of Grand Canyon Village, immediately north of Diana Temple, and south of Scorpion Ridge which lies across the opposite side of Granite Gorge. Access is via the Tonto Trail which traverses 270 degrees around the base of the peak.

Geographic entities mentioned:
surface_form: geikie peak
instance_of: Mountain
countries: United States
coordinates: lat: 36.13304
lon: -112.26962
Access is via the Tonto Trail which traverses 270 degrees around the base of the peak. Topographic relief is significant as Geikie Peak rises over above the Colorado River in. According to the Köppen climate classification system, Geikie Peak is located in a cold semi-arid climate zone. History.

Geographic entities mentioned:
surface_form: geikie peak
instance_of: Mountain
countries: United States
coordinates: lat: 36.13304
lon: -112.26962
Le Piolit. Le Piolit is a 2,464 m mountain in the Dauphiné Alps close to the cities of Gap and Ancelle in the département of Hautes-Alpes in France.

Geographic entities mentioned:
surface_form: piolit
instance_of: Mountain
countries: France
coordinates: lat: 44.60333333
lon: 6.26694444
surface_form: le piolit
instance_of: Mountain
countries: France
coordinates: lat: 44.60333333
lon: 6.26694444
Village of Aigani. The largest settlement in the community is the eponymous mountain village of Aigani. The village is located at an altitude of around on the southeastern face of the foothills of Mount Olympus overlooking the Pineios river delta and Thermaikos Gulf. The area has been an active human settlement since at least the middle Byzantine period.

Geographic entities mentioned:
surface_form: Mount Olympus
instance_of: Mountain
countries: Greece
coordinates: lat: 40.083333333333336
lon: 22.35
Lake Nojiri Naumann Elephant Museum. opened on the shore of Lake Nojiri in Shinano, Nagano Prefecture, Japan, in 1984. Initially the, it was renamed the Lake Nojiri Naumann Elephant Museum in 1996.

Geographic entities mentioned:
surface_form: Lake Nojiri
instance_of: Lake
countries: Japan
coordinates: lat: 36.826388888888886
lon: 138.22194444444443
Kosovo. On 19 March 2018. Taipi received a call-up from Kosovo for the friendly matches against Madagascar and Burkina Faso. On 27 March 2018, he made his debut with Kosovo in a friendly match against Burkina Faso after being named in the starting line-up and he is the third player that comes from the Preševo Valley after Atdhe Nuhiu and Fidan Aliti.

Geographic entities mentioned:
surface_form: Preševo Valley
instance_of: Valley
countries: Serbia
coordinates: lat: 42.3
lon: 21.633333333333
Alcamarina. Alcamarina (possibly from Aymara and Quechua &quot;allqamari&quot; mountain caracara, &quot;-na&quot; a Quechua suffix, may be &quot;the place of the mountain caracara&quot;) is a mountain in the Vilcanota mountain range in the Andes of Peru. It is situated in the Cusco Region, Canchis Province, Pitumarca District. Alcamarina lies northwest of Orco Puñuna and west of Othaña.

Geographic entities mentioned:
surface_form: Orco Puñuna
instance_of: Mountain
countries: Peru
coordinates: lat: -13.9139
lon: -71.1436
surface_form: Othaña
instance_of: Mountain
countries: Peru
coordinates: lat: -13.8997
lon: -71.1444
surface_form: othaña
instance_of: Mountain
countries: Peru
coordinates: lat: -13.8997
lon: -71.1444
Alcamarina. Alcamarina (possibly from Aymara and Quechua &quot;allqamari&quot; mountain caracara, &quot;-na&quot; a Quechua suffix, may be &quot;the place of the mountain caracara&quot;) is a mountain in the Vilcanota mountain range in the Andes of Peru. It is situated in the Cusco Region, Canchis Province, Pitumarca District. Alcamarina lies northwest of Orco Puñuna and west of Othaña.

Geographic entities mentioned:
surface_form: alcamarina
instance_of: Mountain
countries: Peru
coordinates: lat: -13.89972222
lon: -71.15305556
The company develops, manufactures and markets infrared (IR) optics and laser measurement equipment. Founded in 1976, the company was traded on the Tel Aviv Stock Exchange from 1991 until it was acquired, and was a constituent of its Tel-tech index. Headquartered in the Har Hotzvim industrial park in Jerusalem, Israel Ophir owns a complex that includes the group's main production plant.

Geographic entities mentioned:
surface_form: Har Hotzvim
instance_of: Mountain
countries: Israel
coordinates: lat: 31.802527777778
lon: 35.209636111111
The summit is not very visible, including from the road surrounding the summit of Praděd mountain (the summit is slightly to the left below the line of sight to peak). From another characteristic viewpoint – the road around the summit of Dlouhé stráně mountain – it is not visible due to being obscured by mountain. Javorový vrch is visible, among other places, from the pass located near it. Slopes.

Geographic entities mentioned:
surface_form: Dlouhé stráně
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.07125
lon: 17.15675
450 from Bělá pod Pradědem to Bruntál and no. 451 from Nové Heřminovy to Vidly. It is located on a side ridge of the Orlík Massif, between and Mrazový vrch to Nad Borovým. The summit is not very visible, including from the road surrounding the summit of Praděd mountain (the summit is slightly to the left below the line of sight to peak).

Geographic entities mentioned:
surface_form: praděd
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.083194444444445
lon: 17.23086111111111
Javorový vrch. Javorový vrch (formerly also known as Osikový vrch or Černá hora;) is a mountain in the Hrubý Jeseník mountain range in the Czech Republic. It has an elevation of above sea level. The summit and the western slopes are located in the municipality of Bělá pod Pradědem and the eastern slopes are located in the territory of Vrbno pod Pradědem. Location.

Geographic entities mentioned:
surface_form: osikový vrch
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.12152777777778
lon: 17.2475
surface_form: javorový vrch
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.12152777777778
lon: 17.2475
surface_form: černá hora
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 48.978888888889
lon: 13.550833333333
Javorový vrch. Javorový vrch (formerly also known as Osikový vrch or Černá hora;) is a mountain in the Hrubý Jeseník mountain range in the Czech Republic. It has an elevation of above sea level. The summit and the western slopes are located in the municipality of Bělá pod Pradědem and the eastern slopes are located in the territory of Vrbno pod Pradědem. Location.

Geographic entities mentioned:
surface_form: javorový vrch
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.12152777777778
lon: 17.2475
Location. Javorový vrch is situated slightly to the northeast of the central part of the Hrubý Jeseník range, in the western area (microregion) known as the, and borders the neighboring microregion called the. The mountain has a dome-shaped summit.

Geographic entities mentioned:
surface_form: javorový vrch
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.12152777777778
lon: 17.2475
The summit is not very visible, including from the road surrounding the summit of Praděd mountain (the summit is slightly to the left below the line of sight to peak). From another characteristic viewpoint – the road around the summit of Dlouhé stráně mountain – it is not visible due to being obscured by mountain. Javorový vrch is visible, among other places, from the pass located near it. Slopes.

Geographic entities mentioned:
surface_form: javorový vrch
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.12152777777778
lon: 17.2475
Geologically, the massif of Javorový vrch belongs to the unit and is composed of metamorphic rocks, mainly blasto-mylonites (biotites, chlorites, and muscovites), igneous rocks, mainly meta-granitoids, and sedimentary rocks, mainly meta-conglomerates. Waters.

Geographic entities mentioned:
surface_form: javorový vrch
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.12152777777778
lon: 17.2475
The waters from this part of the Hrubý Jeseník range flow into the Oder river basin, fed by mountain streams near the mountain, including the Bělá, Skalní potok, Střední Opava, and Česnekový potok streams. Several short, unnamed streams, tributaries of the Skalní potok and Česnekový potok streams, originate from the slopes of Javorový vrch.

Geographic entities mentioned:
surface_form: javorový vrch
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.12152777777778
lon: 17.2475
450 from Bělá pod Pradědem to Bruntál and no. 451 from Nové Heřminovy to Vidly. It is located on a side ridge of the Orlík Massif, between and Mrazový vrch to Nad Borovým. The summit is not very visible, including from the road surrounding the summit of Praděd mountain (the summit is slightly to the left below the line of sight to peak).

Geographic entities mentioned:
surface_form: orlík
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.176611111111114
lon: 17.29875
Geography. The average altitude in the Isfahan city area is above sea level (compared to 1563 meters for the larger Isfahan province). Mount Soffeh is the highest point in the city at 2216 meters above sea level. The city of Isfahan covers an area of 550 square kilometers and is surrounded by an additional 136 square kilometers in suburbs. Biodiversity.

Geographic entities mentioned:
surface_form: Mount Soffeh
instance_of: Mountain
countries: Iran
coordinates: lat: 32.59222222222222
lon: 51.636944444444445
state of Montana. Lying just east of the Continental Divide in the Many Glacier region of the park, the peak is flanked to the northwest by Swiftcurrent Glacier and to the south by Grinnell Glacier. Mount Grinnell is named after George Bird Grinnell. From the Many Glacier Hotel on Swiftcurrent Lake, the eastern arm of Mount Grinnell, known as Grinnell Point, hides the main summit.

Geographic entities mentioned:
surface_form: Swiftcurrent Lake
instance_of: Lake
countries: United States
coordinates: lat: 48.795277777778
lon: -113.66138888889
surface_form: mount grinnell
instance_of: Mountain
countries: United States
coordinates: lat: 48.7766
lon: -113.727
Mount Grinnell. Mount Grinnell is a peak located in the heart of Glacier National Park in the U.S. state of Montana. Lying just east of the Continental Divide in the Many Glacier region of the park, the peak is flanked to the northwest by Swiftcurrent Glacier and to the south by Grinnell Glacier. Mount Grinnell is named after George Bird Grinnell.

Geographic entities mentioned:
surface_form: mount grinnell
instance_of: Mountain
countries: United States
coordinates: lat: 48.7766
lon: -113.727
state of Montana. Lying just east of the Continental Divide in the Many Glacier region of the park, the peak is flanked to the northwest by Swiftcurrent Glacier and to the south by Grinnell Glacier. Mount Grinnell is named after George Bird Grinnell. From the Many Glacier Hotel on Swiftcurrent Lake, the eastern arm of Mount Grinnell, known as Grinnell Point, hides the main summit.

Geographic entities mentioned:
surface_form: mount grinnell
instance_of: Mountain
countries: United States
coordinates: lat: 48.7766
lon: -113.727
Blue Mountains (Jamaica). The Blue Mountains are the longest mountain range in Jamaica. They include the island's highest point, Blue Mountain Peak, at 2256 m (7402 ft). From the summit, accessible via a walking track, both the north and south coasts of the island can be seen. On a clear day, the outline of the island of Cuba, away, can also be seen.

Geographic entities mentioned:
surface_form: Blue Mountain Peak
instance_of: Mountain
countries: Jamaica
coordinates: lat: 18.046666666667
lon: -76.579166666667
Today, the famous Jamaican Blue Mountain Coffee, which commands premium prices on world markets, is cultivated between and above sea level, while higher slopes are preserved as forest. Hagley Gap and Mavis Bank are farming communities located on Blue Mountain, with Hagley Gap being closest to Blue Mountain Peak. Both towns rely upon the area's rich soil for growing coffee.

Geographic entities mentioned:
surface_form: Blue Mountain Peak
instance_of: Mountain
countries: Jamaica
coordinates: lat: 18.046666666667
lon: -76.579166666667
Big Island Lake (California). Big Island Lake is a lake in Yosemite National Park, United States. Big Island Lake was named from the large lake island it contains.

Geographic entities mentioned:
surface_form: yosemite
instance_of: Valley
countries: United States
coordinates: lat: 37.721694444444445
lon: -119.646
surface_form: island lake
instance_of: Lake
countries: United States
coordinates: lat: 44.38027778
lon: -96.00888889
surface_form: island lake
instance_of: Lake
countries: United States
coordinates: lat: 40.615
lon: -115.381
surface_form: big island lake
instance_of: Lake
countries: United States
coordinates: lat: 38.091
lon: -119.7
surface_form: island lake
instance_of: Lake
countries: United States
coordinates: lat: 46.73416667
lon: -93.19
surface_form: island lake
instance_of: Lake
countries: United States
coordinates: lat: 42.5181
lon: -122.238
surface_form: island lake
instance_of: Lake
countries: United States
coordinates: lat: 47.78027778
lon: -95.02888889
surface_form: island lake
instance_of: Lake
countries: United States
coordinates: lat: 47.6819019
lon: -122.6602552
Big Island Lake (California). Big Island Lake is a lake in Yosemite National Park, United States. Big Island Lake was named from the large lake island it contains.

Geographic entities mentioned:
surface_form: island lake
instance_of: Lake
countries: United States
coordinates: lat: 44.38027778
lon: -96.00888889
surface_form: island lake
instance_of: Lake
countries: United States
coordinates: lat: 40.615
lon: -115.381
surface_form: big island lake (california)
instance_of: Lake
countries: United States
coordinates: lat: 38.091
lon: -119.7
surface_form: island lake
instance_of: Lake
countries: United States
coordinates: lat: 46.73416667
lon: -93.19
surface_form: island lake
instance_of: Lake
countries: United States
coordinates: lat: 42.5181
lon: -122.238
surface_form: island lake
instance_of: Lake
countries: United States
coordinates: lat: 47.78027778
lon: -95.02888889
surface_form: island lake
instance_of: Lake
countries: United States
coordinates: lat: 47.6819019
lon: -122.6602552