Sarmila/GeoWiki-Features huggingface dataset:
The ranch was named after its owner, J. B. Whitmire, a rancher in the 1880s. Its headquarters was located nearby Whitmire Spring on the western shore near the center of Playas Lake. History. The vicinity of Playas Lake was not settled by Americans until near the end of the Apache Wars, although what became known as Whitmire Spring was used as a watering spot and camp by the expedition of Lt. Col.

Geographic entities mentioned:
surface_form: Playas Lake
instance_of: Lake
countries: United States
coordinates: lat: 31.87416667
lon: -108.58555556
Wān Mae Aw. Wān Mae Aw, is a village in Langkho Township, Langkho District, southern Shan State. Geography. Wān Mae Aw lies by the Nam Na-mon River in a mountainous area, 4 km to the east of Loi Lan mountain and 5 km west from Wān Na-mon, a small town near the border with Mae Hong Son Province of Thailand.

Geographic entities mentioned:
surface_form: Loi Lan
instance_of: Mountain
countries: Myanmar
coordinates: lat: 19.64472222
lon: 97.88555556
Lake Rousseau. Lake Rousseau is a reservoir on the Withlacoochee River in central Florida, on the boundary of Levy County to the north-west, Marion County to the north-east, and Citrus County to the south. It was created in the early 1900s when the river was dammed. Florida Power Corp operated a hydroelectric plant from 1909 to 1965 at the western end of the lake.

Geographic entities mentioned:
surface_form: lake rousseau
instance_of: Lake
countries: United States
coordinates: lat: 29.0253
lon: -82.5794
As well as forming part of the Withlacoochee River, it is also fed by the Rainbow River and Lake Panasoffkee to the east. It is approximately twelve miles long by one mile wide, covering an area of c. 3,700 acres (15 km2). To the west is part of the uncompleted Cross Florida Barge Canal leading to the Gulf. The lake forms the centerpiece for the Lake Rousseau State Recreation Area and Campground.

Geographic entities mentioned:
surface_form: lake rousseau
instance_of: Lake
countries: United States
coordinates: lat: 29.0253
lon: -82.5794
The Lamoille Organization Camp, also known as Camp Lamoille and Elko Lion's Club Camp Lamoille, is a camping facility within the Ruby Mountains Ranger District of the Humboldt-Toiyabe National Forest. It was originally constructed in 1939. It is located in Lamoille Canyon, the largest valley of the Ruby Mountains, in Elko County, Nevada. It was a work of the Region 4 of the U.S. Forest Service.

Geographic entities mentioned:
surface_form: Lamoille Canyon
instance_of: Valley
countries: United States
coordinates: lat: 40.6916
lon: -115.474
History. The festival has developed as one of the premier cultural events in Tasmania's arts calendar. Every year on the second weekend in January, the small village of Cygnet, situated in the Huon Valley in the bay of Port Cygnet, presents a variety of music, dance, and related arts, over three days. Performances take place in the pubs, halls, cafes, churches, parks and streets of Cygnet.

Geographic entities mentioned:
surface_form: Huon Valley
instance_of: Valley
countries: Australia
coordinates: lat: -43.12
lon: 146.43
Lamberts Peak. Lamberts Peak () is a small peak north-northeast of the Mason Peaks in the Grove Mountains of Antarctica. It was mapped from air photos, 1956–60, by Australian National Antarctic Research Expeditions, and was named by the Antarctic Names Committee of Australia for G.

Geographic entities mentioned:
surface_form: Mason Peaks
instance_of: Mountain
coordinates: lat: -72.7667
lon: 74.7333
surface_form: small
instance_of: Mountain
coordinates: lat: -70.5
lon: 64.7
surface_form: lamberts peak
instance_of: Mountain
coordinates: lat: -72.7333
lon: 74.85
Lamberts Peak. Lamberts Peak () is a small peak north-northeast of the Mason Peaks in the Grove Mountains of Antarctica. It was mapped from air photos, 1956–60, by Australian National Antarctic Research Expeditions, and was named by the Antarctic Names Committee of Australia for G.

Geographic entities mentioned:
surface_form: lamberts peak
instance_of: Mountain
coordinates: lat: -72.7333
lon: 74.85
Jirisan (TV series). &quot;Jirisan&quot; () is a 2021 South Korean television series starring Jun Ji-hyun and Ju Ji-hoon. It is named after the eponymous mountain in South Korea and has been promoted as &quot;tvN's 15th Anniversary Special Drama&quot;. It premiered on tvN on October 23 to December 12, 2021, and aired every Saturday and Sunday at 21:00 (KST).

Geographic entities mentioned:
surface_form: eponymous mountain
instance_of: Mountain
countries: South Korea
coordinates: lat: 35.336944444444
lon: 127.73055555556
The series is available for streaming on iQIYI worldwide, and on Viki and Netflix in selected territories. Synopsis. Set against the backdrop of towering views of Jirisan, it depicts the story of rangers and other employees of the Jirisan National Park who climb through the mysterious and unexplored regions of the mountain, trying to rescue the survivors and lost trekkers.

Geographic entities mentioned:
surface_form: Jirisan
instance_of: Mountain
countries: South Korea
coordinates: lat: 35.336944444444
lon: 127.73055555556
Cuberant Lake. Cuberant Lake (or Cuberant Lake #1) is a lake in the Uinta Mountains in Summit County, Utah, United States. It is also within the Kamas Ranger District of the Uinta-Wasatch-Cache National Forest and about northwest of Mount Marsell (elevation:). The lake has an elevation of. Cuberant is a word derived from the Ute language meaning &quot;long&quot;.

Geographic entities mentioned:
surface_form: Mount Marsell
instance_of: Mountain
countries: United States
coordinates: lat: 40.731111111111
lon: -110.90805555556
(The Lofty Lake Trail [#158] begins at the Mirror Lake Scenic Byway <a href="Utah_State_Route_150">a></a> and heads northwest through Reid's Meadow before the two trails split.)

Geographic entities mentioned:
surface_form: mirror lake
instance_of: Lake
countries: United States
coordinates: lat: 43.6217
lon: -71.2639
surface_form: mirror lake
instance_of: Lake
countries: United States
coordinates: lat: 39.998
lon: -83.0143
surface_form: mirror lake
instance_of: Lake
countries: United States
coordinates: lat: 27.275555555556
lon: -81.360555555556
surface_form: mirror lake
instance_of: Lake
countries: United States
coordinates: lat: 44.28839
lon: -73.98187
surface_form: mirror lake
instance_of: Lake
countries: United States
coordinates: lat: 40.70458611
lon: -110.88818611
surface_form: mirror lake
instance_of: Lake
countries: United States
coordinates: lat: 45.297063
lon: -121.793134
Cuberant Lake. Cuberant Lake (or Cuberant Lake #1) is a lake in the Uinta Mountains in Summit County, Utah, United States. It is also within the Kamas Ranger District of the Uinta-Wasatch-Cache National Forest and about northwest of Mount Marsell (elevation:). The lake has an elevation of. Cuberant is a word derived from the Ute language meaning &quot;long&quot;.

Geographic entities mentioned:
surface_form: cuberant lake
instance_of: Lake
countries: United States
coordinates: lat: 40.7392574
lon: -110.9144587
Cuberant Lake. Cuberant Lake (or Cuberant Lake #1) is a lake in the Uinta Mountains in Summit County, Utah, United States. It is also within the Kamas Ranger District of the Uinta-Wasatch-Cache National Forest and about northwest of Mount Marsell (elevation:). The lake has an elevation of. Cuberant is a word derived from the Ute language meaning &quot;long&quot;.

Geographic entities mentioned:
surface_form: cuberant lake
instance_of: Lake
countries: United States
coordinates: lat: 40.7392574
lon: -110.9144587
surface_form: cuberant lake
instance_of: Lake
countries: United States
coordinates: lat: 40.7392574
lon: -110.9144587
The (main) lake is substantially larger than the other six lakes in the Cuberant Lakes Basin (the other six are unnamed and are simply referred to as &quot;Cuberant Lake #2&quot;, &quot;Cuberrant Lake #3&quot;, etc.) The Cuberant Lakes Basin drains by way of fairly short stream (about) that flows west-southwest, while descending nearly, and empties into the Weber River.

Geographic entities mentioned:
surface_form: cuberant lake
instance_of: Lake
countries: United States
coordinates: lat: 40.7392574
lon: -110.9144587
As the basin is surrounded by steep inclines and declines, the only reasonable access to the lake and the basin is by way of a trail (#080) the branches off the Lofty Lake Trail and circles around the west side of Mount Marsell.

Geographic entities mentioned:
surface_form: mount marsell
instance_of: Mountain
countries: United States
coordinates: lat: 40.731111111111
lon: -110.90805555556
South Fox Island Light. The South Fox Island Light was a light station located on South Fox Island in the north end of Lake Michigan. There are two towers standing at the site: the first is the original brick keeper's house and tower, while the second is a skeletal tower moved to this site from Sapelo Island, Georgia in 1934. Neither is operational.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Geography. At its fullest length, the river runs from the lake Aursunden in Røros Municipality in Trøndelag county and runs into the Oslofjord at the town of Fredrikstad in Fredrikstad Municipality in Østfold county. Major tributaries include the Vorma River, which drains Lake Mjøsa, joining the Glomma River at Årnes in Nes Municipality.

Geographic entities mentioned:
surface_form: Aursunden
instance_of: Lake
countries: Norway
coordinates: lat: 62.6678
lon: 11.6448
Geography. At its fullest length, the river runs from the lake Aursunden in Røros Municipality in Trøndelag county and runs into the Oslofjord at the town of Fredrikstad in Fredrikstad Municipality in Østfold county. Major tributaries include the Vorma River, which drains Lake Mjøsa, joining the Glomma River at Årnes in Nes Municipality.

Geographic entities mentioned:
surface_form: Lake Mjøsa
instance_of: Lake
countries: Norway
coordinates: lat: 60.666666666667
lon: 11
Major tributaries include the Vorma River, which drains Lake Mjøsa, joining the Glomma River at Årnes in Nes Municipality. The large river Lågen flows into Lake Mjøsa, draining the large Gudbrandsdalen valley and significantly increasing the Glomma's flow. Because it flows through some of the richest forest districts, it has historically been Norway's leading log-floating river.

Geographic entities mentioned:
surface_form: Gudbrandsdalen
instance_of: Valley
countries: Norway
coordinates: lat: 61.1333
lon: 10.35
Some of the country's largest manufacturing and processing concerns are found around its mouth, where supplies of timber and hydropower have been backed by excellent port facilities. The upper limit of the Glomma valley farms is variable, but typically runs about in Østerdalen, slightly lower than in the Gudbrandsdalen, which reflects the colder climate.

Geographic entities mentioned:
surface_form: Glomma valley
instance_of: Valley
countries: Norway
surface_form: Østerdalen
instance_of: Valley
countries: Norway
coordinates: lat: 61.575916666666664
lon: 11.087111111111112
The treeline, with a light birch forest, rises to about in Østerdalen. North of Røros, the forested areas are only on the valley floor. The upper river valleys of Norwegian rivers have distinctive names which are vestiges of earlier cultural distinctions such as building styles, traditional clothing or bunad and domestic crafts. The upper valley of the Glomma is the Østerdalen ().

Geographic entities mentioned:
surface_form: Østerdalen
instance_of: Valley
countries: Norway
coordinates: lat: 61.575916666666664
lon: 11.087111111111112
Camp Pine Knot. Camp Pine Knot, also known as Huntington Memorial Camp, on Raquette Lake in the Adirondack Mountains of New York State, was built by William West Durant. Begun in 1877, it was the first of the &quot;Adirondack Great Camps&quot; and epitomizes the &quot;Great Camp&quot; architectural style.

Geographic entities mentioned:
surface_form: Raquette Lake
instance_of: Lake
countries: United States
coordinates: lat: 43.833333333333
lon: -74.65
Tanjombato. Tanjombato is a suburb and a rural municipality of Antananarivo in the Analamanga Region (Central Highlands of Madagascar). It belongs to the district of Antananarivo-Atsimondrano and had a population of 50,373 as of 2018. It is situated at 7 km South from downtown Antananarivo and is crossed by the Ikopa River and the National Road 7.

Geographic entities mentioned:
surface_form: Ikopa River
instance_of: Watercourse
countries: Madagascar
coordinates: lat: -16.798611111111
lon: 46.855555555556
Manappalli. Manapalli is a small village on the northern bank of the Cauvery River in the Namakkal district of Tamil Nadu, India.

Geographic entities mentioned:
surface_form: Cauvery River
instance_of: Watercourse
countries: India
coordinates: lat: 11.370345
lon: 79.828105
On its coast, there is a flowing river rich in fruit-bearing trees. It also has a safe and well-frequented harbor.&quot;
At the beginning of the 16th century, Nedroma became an important textile center, specializing in cotton wovens and blankets. Nedroma, although far from Algiers, was an administrative center of the Trara, extending its influence to neighboring towns.

Geographic entities mentioned:
surface_form: Trara
instance_of: Mountain
countries: Algeria
France
There is an outlet on the southeast shore of the lake that leads through a small stream (also called Grindstone Creek) to Lac Courte Oreilles. There is a small island in the west corner named TTI.

Geographic entities mentioned:
surface_form: Lac Courte Oreilles
instance_of: Lake
countries: United States
coordinates: lat: 45.883333333333
lon: -91.416666666667
There is a small island in the west corner named TTI. Grindstone Lake is located approximately six miles southeast of the city of Hayward, the primary commercial and retail center of the area, and is one of three large natural lakes (Lac Courte Oreilles, Grindstone Lake, and Round Lake) located to the south and east of the city.

Geographic entities mentioned:
surface_form: Lac Courte Oreilles
instance_of: Lake
countries: United States
coordinates: lat: 45.883333333333
lon: -91.416666666667
surface_form: grindstone lake
instance_of: Lake
countries: United States
coordinates: lat: 45.9333
lon: -91.4167
surface_form: grindstone lake
instance_of: Lake
countries: United States
coordinates: lat: 45.9333
lon: -91.4167
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 43.9344286
lon: -96.9790408
surface_form: round lake
instance_of: Body of water
countries: United States
coordinates: lat: 44.0648
lon: -75.1033
The first known visit by Europeans to the area was around 1659 when Pierre-Esprit Radisson and Médard des Groseilliers travelled from Chequamegon Bay on Lake Superior southward through the area and stayed for a period at an Indian village that has been identified as being located on the nearby Lac Courte Oreilles.

Geographic entities mentioned:
surface_form: Lac Courte Oreilles
instance_of: Lake
countries: United States
coordinates: lat: 45.883333333333
lon: -91.416666666667
Grindstone Lake was apparently well travelled by Indians and early traders and explorers who used it as part of the route from Lac Courte Oreilles (in the Chippewa River watershed), through Grindstone Lake and Windigo Lake and over the Namekagon Portage, to the Namekagon River (in the St. Croix River watershed).

Geographic entities mentioned:
surface_form: Lac Courte Oreilles
instance_of: Lake
countries: United States
coordinates: lat: 45.883333333333
lon: -91.416666666667
surface_form: Windigo Lake
instance_of: Lake
countries: United States
coordinates: lat: 45.930277777778
lon: -91.47
surface_form: grindstone lake
instance_of: Lake
countries: United States
coordinates: lat: 45.9333
lon: -91.4167
Croix River watershed). A later explorer, Jonathan Carver, passed through the area in 1767 and (on his way from the Indian village on Lac Courte Oreilles to the Namekagon River) specifically travelled through what the editor identifies as Grindstone Lake on June 29, 1767. The area was later visited by Henry Schoolcraft in 1831 who described crossing from the St.

Geographic entities mentioned:
surface_form: Lac Courte Oreilles
instance_of: Lake
countries: United States
coordinates: lat: 45.883333333333
lon: -91.416666666667
surface_form: grindstone lake
instance_of: Lake
countries: United States
coordinates: lat: 45.9333
lon: -91.4167
Croix River watershed). A later explorer, Jonathan Carver, passed through the area in 1767 and (on his way from the Indian village on Lac Courte Oreilles to the Namekagon River) specifically travelled through what the editor identifies as Grindstone Lake on June 29, 1767. The area was later visited by Henry Schoolcraft in 1831 who described crossing from the St.

Geographic entities mentioned:
surface_form: Windigo Lake
instance_of: Lake
countries: United States
coordinates: lat: 45.930277777778
lon: -91.47
surface_form: Lac Courte Oreilles
instance_of: Lake
countries: United States
coordinates: lat: 45.883333333333
lon: -91.416666666667
surface_form: grindstone lake
instance_of: Lake
countries: United States
coordinates: lat: 45.9333
lon: -91.4167
Grindstone Lake (Wisconsin). Geographical and general information. Grindstone Lake is a large freshwater lake located in north central Wisconsin in the Town of Bass Lake, Sawyer County, United States, in township 40 north, ranges 8 and 9 west. The lake is roughly oval shaped being approximately three miles in length east to west and two miles (3 km) north to south.

Geographic entities mentioned:
surface_form: grindstone lake
instance_of: Lake
countries: United States
coordinates: lat: 45.9333
lon: -91.4167
Grindstone Lake is a large freshwater lake located in north central Wisconsin in the Town of Bass Lake, Sawyer County, United States, in township 40 north, ranges 8 and 9 west. The lake is roughly oval shaped being approximately three miles in length east to west and two miles (3 km) north to south. Grindstone Lake is in size (including islands) with a maximum depth of and a shoreline of.

Geographic entities mentioned:
surface_form: grindstone lake
instance_of: Lake
countries: United States
coordinates: lat: 45.9333
lon: -91.4167
The eastern part of the lake is located in the Lac Courte Oreilles Indian Reservation. The shore of the lake is principally occupied by seasonal lake cabins and homes. There are two public boat landings on Grindstone Lake: an improved landing at the southwest corner and a small, unimproved landing at the southeast corner near the outlet stream.

Geographic entities mentioned:
surface_form: grindstone lake
instance_of: Lake
countries: United States
coordinates: lat: 45.9333
lon: -91.4167
A large commercial Cranberry bog was formerly located on the southwest shore of the lake near the improved boat landing but has now been closed. Grindstone Lake is a popular resort area drawing cabin owners and visitors from the Minneapolis-St. Paul, Milwaukee, and Chicago metropolitan areas. Origin of name.

Geographic entities mentioned:
surface_form: grindstone lake
instance_of: Lake
countries: United States
coordinates: lat: 45.9333
lon: -91.4167
Paul, Milwaukee, and Chicago metropolitan areas. Origin of name. The Dictionary of Wisconsin History states that the name &quot;Grindstone Lake&quot; originates from the Chippewa word &quot;Gaa-zhiigwanaabikokaag&quot; meaning &quot;a place abundant with grindstones.&quot; However, the lake has not always been referred to as &quot;Grindstone Lake&quot; in the past.

Geographic entities mentioned:
surface_form: grindstone lake
instance_of: Lake
countries: United States
coordinates: lat: 45.9333
lon: -91.4167
surface_form: grindstone lake
instance_of: Lake
countries: United States
coordinates: lat: 45.9333
lon: -91.4167
Captain James Allen who accompanied Schoolcraft on an expedition in the following year (1832) to the source of the Mississippi River produced a detailed map of the northern Minnesota/Wisconsin area after that trip. On this map he labels Grindstone Lake in English as &quot;Sandstone Lake.&quot;
History. Prior to European exploration, the area of Grindstone Lake was inhabited by the Ojibwa Indians.

Geographic entities mentioned:
surface_form: grindstone lake
instance_of: Lake
countries: United States
coordinates: lat: 45.9333
lon: -91.4167
Geology. The lakes are maars or low-profile volcanic craters located in the San Pablo Volcanic Field. They are among the 200 small monogenetic volcanoes found along the Macolod Corridor, a rift zone between Mount Makiling and Mount Banahaw, which is part of the larger Southwestern Luzon Volcanic Field.

Geographic entities mentioned:
surface_form: Mount Makiling
instance_of: Mountain
countries: Philippines
coordinates: lat: 14.13
lon: 121.2
surface_form: Mount Banahaw
instance_of: Mountain
countries: Philippines
coordinates: lat: 14.066666666667
lon: 121.48333333333
Then US 41 and US 76 becomes East Main Street in downtown Chattanooga up to the intersection with Broad Street (US 11 and US 64). At that point US 76 terminates, US 72 begins, and the now-conjoined US 41 and US 72 merges with US 11 and US 64, trekking southwestward around the base of Lookout Mountain into the Tiftonia community.

Geographic entities mentioned:
surface_form: Lookout Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 34.863713888889
lon: -85.392452777778
Just west of Tiftonia, US 11 splits off, and it veers southwestward into Georgia. US 41, US 64, and US 72 take a westward path from Hamilton County into Marion County. US 41 breaks off from US 64 and US 72 at Jasper and joins with unsigned SR 150 before ascending the Cumberland Plateau. US 41 leaves SR 150 and joins with SR 56 at Tracy City and runs southwest into Monteagle.

Geographic entities mentioned:
surface_form: Cumberland Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 36
lon: -85
Bangadi. Bangadi is a town located in Haut-Uele Province, Democratic Republic of the Congo. History. During Belgian colonial rule, Bangadi was an important town. After the Duru September 2008 attack, the town residents established a self-defense group due to their distrust of the government. On 8 October, 120 self-defense group militias attacked the town police station and gained few firearms.

Geographic entities mentioned:
surface_form: bangadi
instance_of: Watercourse
countries: Democratic Republic of the Congo
coordinates: lat: 4.74218
lon: 26.88968
After the Duru September 2008 attack, the town residents established a self-defense group due to their distrust of the government. On 8 October, 120 self-defense group militias attacked the town police station and gained few firearms. LRA attacked Bangadi on 19 October, killing 9 and abducting 41 children. They looted and burned houses and pillaged a health center.

Geographic entities mentioned:
surface_form: bangadi
instance_of: Watercourse
countries: Democratic Republic of the Congo
coordinates: lat: 4.74218
lon: 26.88968
Nevertheless, the town residents defeated them before reaching the central market. Due to the attack, the residents fled to the bush. During the Christmas massacres, LRA killed 48 people in Bangadi areas. LRA stormed Bangadi on 22 January 2009 and the town self-defense group repelled the attack and chased them to the outskirts of the town.

Geographic entities mentioned:
surface_form: bangadi
instance_of: Watercourse
countries: Democratic Republic of the Congo
coordinates: lat: 4.74218
lon: 26.88968
Due to the attack, the residents fled to the bush. During the Christmas massacres, LRA killed 48 people in Bangadi areas. LRA stormed Bangadi on 22 January 2009 and the town self-defense group repelled the attack and chased them to the outskirts of the town. Two days later, FARDC sent 175 soldiers from the 911th Battalion to the town.

Geographic entities mentioned:
surface_form: bangadi
instance_of: Watercourse
countries: Democratic Republic of the Congo
coordinates: lat: 4.74218
lon: 26.88968
Two days later, FARDC sent 175 soldiers from the 911th Battalion to the town. The Bangadi self-defense group was abolished in June 2009 due to the order of Major Nelson Mugaba. In December 2009, the 911th Battalion departed from Bangadi and was replaced by the 912th Battalion. Education. The town has a primary school. Healthcare. There is a health center in the town.

Geographic entities mentioned:
surface_form: bangadi
instance_of: Watercourse
countries: Democratic Republic of the Congo
coordinates: lat: 4.74218
lon: 26.88968
History. During Belgian colonial rule, Bangadi was an important town. After the Duru September 2008 attack, the town residents established a self-defense group due to their distrust of the government. On 8 October, 120 self-defense group militias attacked the town police station and gained few firearms. LRA attacked Bangadi on 19 October, killing 9 and abducting 41 children.

Geographic entities mentioned:
surface_form: duru
instance_of: Watercourse
countries: Democratic Republic of the Congo
coordinates: lat: 3.7491666666667
lon: 28.044722222222
Lake Peipus. Lake Peipus is the largest trans-boundary lake in Europe, lying on the international border between Estonia and Russia. The lake is the fifth-largest in Europe after Lake Ladoga and Lake Onega (in Russia), Lake Vänern (in Sweden), and Lake Saimaa (in Finland). The lake is used for fishing and recreation, but suffered from environmental degradation from Soviet-era agriculture.

Geographic entities mentioned:
surface_form: Lake Ladoga
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 60.842777777777776
lon: 31.459722222222222
surface_form: Lake Onega
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 61.690555555556
lon: 35.655555555556
surface_form: Lake Vänern
instance_of: Lake
countries: Sweden
coordinates: lat: 58.916666666667
lon: 13.5
Lake Peipus. Lake Peipus is the largest trans-boundary lake in Europe, lying on the international border between Estonia and Russia. The lake is the fifth-largest in Europe after Lake Ladoga and Lake Onega (in Russia), Lake Vänern (in Sweden), and Lake Saimaa (in Finland). The lake is used for fishing and recreation, but suffered from environmental degradation from Soviet-era agriculture.

Geographic entities mentioned:
surface_form: peipus
instance_of: Lake
countries: Estonia
Russia
Russian Empire
Soviet Union
coordinates: lat: 58.676666666667
lon: 27.491666666667
surface_form: lake peipus
instance_of: Lake
countries: Estonia
Russia
Russian Empire
Soviet Union
coordinates: lat: 58.676666666667
lon: 27.491666666667
The lake is used for fishing and recreation, but suffered from environmental degradation from Soviet-era agriculture. Some 30 rivers and streams discharge into Lake Peipus, the two largest of which are the Velikaya and Emajõgi. The lake drains into the Gulf of Finland via the Narva River.

Geographic entities mentioned:
surface_form: peipus
instance_of: Lake
countries: Estonia
Russia
Russian Empire
Soviet Union
coordinates: lat: 58.676666666667
lon: 27.491666666667
surface_form: lake peipus
instance_of: Lake
countries: Estonia
Russia
Russian Empire
Soviet Union
coordinates: lat: 58.676666666667
lon: 27.491666666667
Some 30 rivers and streams discharge into Lake Peipus, the two largest of which are the Velikaya and Emajõgi. The lake drains into the Gulf of Finland via the Narva River. On 5 April 1242, the frozen lake was the site of the Battle on the Ice (also known as the Battle of Lake Peipus) between the armies of the Novgorod Republic and the Teutonic Order. Name.

Geographic entities mentioned:
surface_form: peipus
instance_of: Lake
countries: Estonia
Russia
Russian Empire
Soviet Union
coordinates: lat: 58.676666666667
lon: 27.491666666667
surface_form: lake peipus
instance_of: Lake
countries: Estonia
Russia
Russian Empire
Soviet Union
coordinates: lat: 58.676666666667
lon: 27.491666666667
On 5 April 1242, the frozen lake was the site of the Battle on the Ice (also known as the Battle of Lake Peipus) between the armies of the Novgorod Republic and the Teutonic Order. Name. The origin of the name &quot;Peipus&quot; () is uncertain, although it may be paralleled by Lake Peipiä () and the village of Peipiä () along its shore, and by Peipozero () near Onega Bay.

Geographic entities mentioned:
surface_form: peipus
instance_of: Lake
countries: Estonia
Russia
Russian Empire
Soviet Union
coordinates: lat: 58.676666666667
lon: 27.491666666667
Because of the shallow depth, the lake quickly warms and cools. Water temperature reaches in July. The lakes freeze in late November – early December and thaw in late April – early May, first lakes Teploe and Pihkva and then lake Peipus. However, due to recent climatic changes, Lake Peipus has now commonly started to freeze later into December and thaw much earlier in April. Basin and islands.

Geographic entities mentioned:
surface_form: peipus
instance_of: Lake
countries: Estonia
Russia
Russian Empire
Soviet Union
coordinates: lat: 58.676666666667
lon: 27.491666666667
surface_form: peipus
instance_of: Lake
countries: Estonia
Russia
Russian Empire
Soviet Union
coordinates: lat: 58.676666666667
lon: 27.491666666667
surface_form: lake peipus
instance_of: Lake
countries: Estonia
Russia
Russian Empire
Soviet Union
coordinates: lat: 58.676666666667
lon: 27.491666666667
surface_form: lake peipus
instance_of: Lake
countries: Estonia
Russia
Russian Empire
Soviet Union
coordinates: lat: 58.676666666667
lon: 27.491666666667
Moulouya River. The Moulouya River () is a river in Morocco. Its sources are located in the Ayashi mountain in the Middle Atlas. It empties into the Mediterranean Sea near Saïdia, in northeast Morocco. Water level in the river often fluctuates. The river is used for irrigation and is dammed by the Hassan II and Mohamed V Dams. History.

Geographic entities mentioned:
surface_form: Ayashi
instance_of: Mountain
countries: Morocco
coordinates: lat: 32.477777777778
lon: -4.9269444444444
Xenotilapia nigrolabiata. &quot;Xenotilapia nigrolabiata&quot; is a species of cichlid endemic to Lake Tanganyika where it prefers areas with sandy substrates. This species can reach a length of TL. It can also be found in the aquarium trade.

Geographic entities mentioned:
surface_form: Lake Tanganyika
instance_of: Lake
countries: Tanzania
Democratic Republic of the Congo
Burundi
Zambia
coordinates: lat: -6.1
lon: 29.5
Guolehis Suolojávri. Guolehis Suolojávri is a lake in Guovdageainnu Municipality in Finnmark county, Norway. The lake lies about west of the lake Suolojávri and about north of the Norway-Finland border.

Geographic entities mentioned:
surface_form: suolojávri
instance_of: Lake
countries: Norway
coordinates: lat: 68.80199
lon: 23.39256
surface_form: guolehis suolojávri
instance_of: Lake
countries: Norway
coordinates: lat: 68.8185
lon: 23.3519
surface_form: suolojávri
instance_of: Lake
countries: Norway
coordinates: lat: 70.361294
lon: 26.094642
Guolehis Suolojávri. Guolehis Suolojávri is a lake in Guovdageainnu Municipality in Finnmark county, Norway. The lake lies about west of the lake Suolojávri and about north of the Norway-Finland border.

Geographic entities mentioned:
surface_form: suolojávri
instance_of: Lake
countries: Norway
coordinates: lat: 68.80199
lon: 23.39256
surface_form: suolojávri
instance_of: Lake
countries: Norway
coordinates: lat: 70.361294
lon: 26.094642
Alwand Dam. Alwand Dam is a dam located on the Alwand River, southeast of Khanaqin, from the Iraqi-Iranian border. It is a hydroponic dam with a mud core with a length of and a height of. The storage quantities in the dam's lake is and the surface area of the lake is. History. At the beginning of 2013, the dam began operating.

Geographic entities mentioned:
surface_form: dam's lake
instance_of: Lake
countries: Iraq
coordinates: lat: 34.31027777777778
lon: 45.45277777777778
He endowed the monasteries at Meteora and eventually became the head of the local monastic community, rebuilding or establishing further monasteries in the area in 1388 and 1390. In the 1390s he visited Mount Athos, but was back in Meteora by 1401, and died there in 1422 or 1423. John Uroš was the last emperor of Serbs and Greeks and the last Serbian ruler of Thessaly.

Geographic entities mentioned:
surface_form: Mount Athos
instance_of: Mountain
countries: Greece
coordinates: lat: 40.15833333333333
lon: 24.327222222222222
The then-Chief General of the Yugoslav Army Nebojša Pavković requested that Mladić vacate the facility where he was staying on mountain Povlen, near Valjevo, after which the Serb military agencies claim to have lost all trace of him. Initially, Mladić lived freely in Belgrade.

Geographic entities mentioned:
surface_form: Povlen
instance_of: Mountain
countries: Serbia
coordinates: lat: 44.132777777778
lon: 19.748888888889
Geography. Aubagne is located in the Huveaune Valley and surrounded by the mountain ranges of Garlaban with Sainte-Baume to the north and east of Marseille. Aubagne was the main city of the former Agglomeration community of Pays d'Aubagne et de l'Étoile; it has been part of the Aix-Marseille-Provence Metropolis since 2016. It is the sixth largest city of Bouches-du-Rhône by population.

Geographic entities mentioned:
surface_form: Garlaban
instance_of: Mountain
countries: France
coordinates: lat: 43.331388888889
lon: 5.5536111111111
On 4 April 1402 in Brantes, at the foot of Mont Ventoux, and in the presence of his wife &quot;Alix des Baux&quot;, Odon de Villars bestowed upon his nephew Philippe de Lévis the fiefs of Brantes, Plaisians and their dependencies: the Lordships of Saint-Marcel, Roquefort, le Castellet, Cassis, and Port-Miou which were dependencies of the barony of Aubagne, as well as La Fare-les-Oliviers, and Éguilles.

Geographic entities mentioned:
surface_form: Mont Ventoux
instance_of: Mountain
countries: France
coordinates: lat: 44.166666666667
lon: 5.2833333333333
Shafter station (Atchison, Topeka and Santa Fe Railway). The Santa Fe Passenger and Freight Depot is a former Santa Fe Railroad station located at 150 Central Valley Highway in Shafter, in the southern San Joaquin Valley within Kern County, California. History. The San Francisco and San Joaquin Valley Railroad was built in the late 1890s and later became the Valley Division of the Santa Fe.

Geographic entities mentioned:
surface_form: San Joaquin Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.628888888889
lon: -120.185
In 1924, the dancer and choreographer Baruch Agadati choreographed a dance based on the Romanian Hora dance that became known as &quot;Hora Agadati&quot;. It was performed by the Ohel Workers' Theatre, which toured pioneer settlements in the Jezreel Valley.

Geographic entities mentioned:
surface_form: Jezreel Valley
instance_of: Valley
countries: Israel
coordinates: lat: 32.596388888889
lon: 35.241944444444
Career. Kingo started his career by working as a private tutor at Frederiksborg Castle. From 1659 he lived on the Vedbygård estate at Tissø, where he wrote some of his first poems. In 1661 he was appointed chaplain to the priest Peder Worm at Kirke Helsinge and Drøsselbjerg, and in 1668 he was ordained a minister in his hometown of Slangerup, where his poem-writing began.

Geographic entities mentioned:
surface_form: Tissø
instance_of: Lake
countries: Denmark
coordinates: lat: 55.57591
lon: 11.29205
Storsjøen (Rendalen). Storsjøen is the ninth-deepest lake in Norway at in depth. The lake lies in Rendalen Municipality and Åmot Municipality which are in Innlandet county, Norway. The lake is long, but only wide at its broadest point. The lake lies above sea level, has an area of, and a volume of.

Geographic entities mentioned:
surface_form: storsjøen
instance_of: Lake
countries: Norway
coordinates: lat: 60.3725
lon: 11.625
surface_form: storsjøen
instance_of: Lake
countries: Norway
coordinates: lat: 61.45222222
lon: 11.30972222
Planned upstream water abstractions include the Matabeleland Zambezi Water Project in Zimbabwe that would bring water from the Zambezi to Bulawayo and its surrounding areas, as well as a proposed extension of the existing North-South Carrier in Botswana that would connect the carrier to the Zambezi River. Zambia and Namibia both have plans to expand irrigation in the upper river basin.

Geographic entities mentioned:
surface_form: Matabeleland Zambezi Water Project
instance_of: Lake
countries: Zimbabwe
coordinates: lat: -18.50722222222222
lon: 27.189444444444444
Crater Peak (Colorado). Crater Peak is the highest summit of Grand Mesa in the Rocky Mountains of North America. The prominent peak is located on the drainage divide separating Grand Mesa National Forest and Gunnison National Forest, north-northwest (bearing 342°) of the Town of Paonia in Delta County, Colorado, United States.

Geographic entities mentioned:
surface_form: Grand Mesa
instance_of: Mountain
countries: United States
coordinates: lat: 39.1333
lon: -107.933
surface_form: crater peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.0397
lon: -107.663
Crater Peak (Colorado). Crater Peak is the highest summit of Grand Mesa in the Rocky Mountains of North America. The prominent peak is located on the drainage divide separating Grand Mesa National Forest and Gunnison National Forest, north-northwest (bearing 342°) of the Town of Paonia in Delta County, Colorado, United States.

Geographic entities mentioned:
surface_form: crater peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.0397
lon: -107.663
Crater Peak (Colorado). Crater Peak is the highest summit of Grand Mesa in the Rocky Mountains of North America. The prominent peak is located on the drainage divide separating Grand Mesa National Forest and Gunnison National Forest, north-northwest (bearing 342°) of the Town of Paonia in Delta County, Colorado, United States.

Geographic entities mentioned:
surface_form: grand mesa
instance_of: Mountain
countries: United States
coordinates: lat: 39.1333
lon: -107.933
Streckelsberg. The Streckelsberg is an approximately 58-metre high coastal cliff on the island of Usedom in North Germany. After the Golm and the Kückelsberg, the Streckelsberg is the third highest elevation on the island. The Streckelsberg is located half a kilometre southeast of the former fishing village and present-day seaside resort of Koserow directly on the Baltic Sea shore.

Geographic entities mentioned:
surface_form: streckelsberg
instance_of: Mountain
countries: Germany
coordinates: lat: 54.052466666667
lon: 14.013780555556
After the Golm and the Kückelsberg, the Streckelsberg is the third highest elevation on the island. The Streckelsberg is located half a kilometre southeast of the former fishing village and present-day seaside resort of Koserow directly on the Baltic Sea shore. To the southeast is the village of Kölpinsee; the B 111 federal road and Usedomer Bäderbahn railway run past the hill to the southwest.

Geographic entities mentioned:
surface_form: streckelsberg
instance_of: Mountain
countries: Germany
coordinates: lat: 54.052466666667
lon: 14.013780555556
To the southeast is the village of Kölpinsee; the B 111 federal road and Usedomer Bäderbahn railway run past the hill to the southwest. Geology. The Streckelsberg was formed during the last ice age as a push moraine. At that time over 16,000 years ago large parts of central and northern Europe were covered by a massive ice sheet.

Geographic entities mentioned:
surface_form: streckelsberg
instance_of: Mountain
countries: Germany
coordinates: lat: 54.052466666667
lon: 14.013780555556
At that time over 16,000 years ago large parts of central and northern Europe were covered by a massive ice sheet. During the gradual retreat of the ice, there were repeated smaller advances of the glacier that led to the formation of moraines. The Streckelsberg was formed during such an advance, when the glacier pushed loose sedimentary rock in front of it, piling it up.

Geographic entities mentioned:
surface_form: streckelsberg
instance_of: Mountain
countries: Germany
coordinates: lat: 54.052466666667
lon: 14.013780555556
When the ice retreated further, the first Baltic proglacial lake was formed from the meltwaters and rising sea levels, later the Yoldia Sea and Ancylus Lake were created and, ultimately, the Baltic Sea in its present shape. Originally, the Streckelsberg was much larger than it is today, both in terms of size and height.

Geographic entities mentioned:
surface_form: streckelsberg
instance_of: Mountain
countries: Germany
coordinates: lat: 54.052466666667
lon: 14.013780555556
Originally, the Streckelsberg was much larger than it is today, both in terms of size and height. Through erosion processes the Streckelsberg soon shrank, particularly as a result of breakers from the Baltic Sea. Wave and wind erosion has reduced the Streckelsberg by in the last 300 years.

Geographic entities mentioned:
surface_form: streckelsberg
instance_of: Mountain
countries: Germany
coordinates: lat: 54.052466666667
lon: 14.013780555556
Through erosion processes the Streckelsberg soon shrank, particularly as a result of breakers from the Baltic Sea. Wave and wind erosion has reduced the Streckelsberg by in the last 300 years. This process still continues, despite coastal protection measures taken in 1995, including groynes, two breakwaters, a triple protective wall and the dumping of artificial sand.

Geographic entities mentioned:
surface_form: streckelsberg
instance_of: Mountain
countries: Germany
coordinates: lat: 54.052466666667
lon: 14.013780555556
In strong storms, parts of the cliff frequently break off and slump down onto the beach. Geological history of the island of Usedom and the Streckelsberg. The landscape of Northern Germany was formed as a result of several cold stages. Huge masses of ice advanced from Scandinavia to central Germany.

Geographic entities mentioned:
surface_form: streckelsberg
instance_of: Mountain
countries: Germany
coordinates: lat: 54.052466666667
lon: 14.013780555556
The Streckelsberg is such a terminal moraine, with an area of sandur to the south as far as the Achterwasser lagoon. The Baltic Sea on the north side of the Streckelsberg can be regarded as a giant terminal moraine lake. 7000 to 5000 years ago the island did not exist in its current form. Only the terminal moraines, also known as island or geest cores stuck out from the waters of the Baltic Sea.

Geographic entities mentioned:
surface_form: streckelsberg
instance_of: Mountain
countries: Germany
coordinates: lat: 54.052466666667
lon: 14.013780555556
There are also young trees of the species Norway Maple, Sycamore and Silver Birch. The tree layer is dominated by beech trees that are more than 180 years old and, on the slopes of the hill, by equally ancient Scots Pines. Afforestation of the Streckelsberg by Senior Forester Schrödter.

Geographic entities mentioned:
surface_form: streckelsberg
instance_of: Mountain
countries: Germany
coordinates: lat: 54.052466666667
lon: 14.013780555556
Afforestation of the Streckelsberg by Senior Forester Schrödter. Senior Forester (&quot;Oberförster&quot;) Schrödter afforested the Streckelsberg in 1818 and 1819 in its present form with beech trees in order to better protect the hill and the village of Koserow behind it from the harsh sea winds and from drifting sand. Schrödter was born in 1753 in Klein Behnitz (in the March of Brandenburg).

Geographic entities mentioned:
surface_form: streckelsberg
instance_of: Mountain
countries: Germany
coordinates: lat: 54.052466666667
lon: 14.013780555556
The main bird species on the Streckelsberg are the robin wren, great tit, blue tit, chiffchaff, red-breasted flycatcher, willow warbler, blackcap and lesser whitethroat. The somewhat larger blackbird and song thrush also live on the Streckelsberg. In the tree layer there are golden oriole, chaffinch, stock dove, tawny owl, wood pigeon, hooded crow and goshawk.

Geographic entities mentioned:
surface_form: streckelsberg
instance_of: Mountain
countries: Germany
coordinates: lat: 54.052466666667
lon: 14.013780555556
Bats also have their summer homes in tree hollows and cracks. Depending on the biodiversity of the flora, many insect species live on Streckelsberg. In addition to various butterflies there are also beetles, including the capricorn beetle, sawyer and longhorn beetle, whose larvae live on dead wood.

Geographic entities mentioned:
surface_form: streckelsberg
instance_of: Mountain
countries: Germany
coordinates: lat: 54.052466666667
lon: 14.013780555556
From the walking trail on the top of the cliffs on the Streckelsberg a wide variety of water birds may be seen including: Mallard, black-headed gull, common gull, herring gull, great black-backed gull, great crested grebe, coot, cormorant and mute swan.

Geographic entities mentioned:
surface_form: streckelsberg
instance_of: Mountain
countries: Germany
coordinates: lat: 54.052466666667
lon: 14.013780555556
The state of the terrain is classified as satisfactory, because parts of it are used for forestry
Koserow Observation Tower. The Koserow Observation Tower was a Wehrmacht observation tower on the Streckelsberg built in the late 1930s for observers of air raids (e.g., on the ports of Swinemünde and Szczecin).

Geographic entities mentioned:
surface_form: streckelsberg
instance_of: Mountain
countries: Germany
coordinates: lat: 54.052466666667
lon: 14.013780555556
Plot. During a climb up Kangchenjunga, a mountaineer named Um Hong-gil (Hwang Jung-min) saves the life of Park Moo-taek (Jung Woo) and his friend Park Jeong-Bok (Kim In-kwon), in the aftermath he warned them never to climb mountains again. A few days later he and his crew got a project and he needs new members.

Geographic entities mentioned:
surface_form: Kangchenjunga
instance_of: Mountain
countries: India
Nepal
coordinates: lat: 27.7
lon: 88.133333
Alongside the beck runs the B5322, St John’s in the Vale Road. The vale is in the heart of the northern Lake District and is surrounded by many of the most striking of the Lakeland fells. It runs from south to north, set between the rocky flanks of Clough Head to the east and the neighbours High Rigg and Low Rigg to the west.

Geographic entities mentioned:
surface_form: Clough Head
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.593261111111
lon: -3.0337888888889
surface_form: High Rigg
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.588430555556
lon: -3.07235
surface_form: Low Rigg
instance_of: Mountain
countries: United Kingdom
It runs from south to north, set between the rocky flanks of Clough Head to the east and the neighbours High Rigg and Low Rigg to the west. The southern end of the vale is a narrow pass between High Rigg and Great Dodd, just to the north of the small settlement of Legburthwaite. At its northern end the vale widens to meet the broad east-to-west valley of the River Greta near Threlkeld.

Geographic entities mentioned:
surface_form: Great Dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.575411111111
lon: -3.0194111111111
At its northern end the vale widens to meet the broad east-to-west valley of the River Greta near Threlkeld. The view north from the vale is dominated by the mountains Blencathra and Skiddaw. High on the western side of the vale lies St John’s in the Vale Church, located in a low pass between High Rigg on the southern side and Low Rigg to the north.

Geographic entities mentioned:
surface_form: Blencathra
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.63985
lon: -3.0504611111111
surface_form: Skiddaw
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.651388888889
lon: -3.1477777777778
St John's in the Vale. St John’s in the Vale is a glacial valley in the Lake District National Park, Cumbria, England. Within the vale are a number of farms and small settlements, in addition to several disused quarry and mining works. St John’s Beck meanders northward along the floor of the vale, and is the main outflow from Thirlmere reservoir, which is located to the south.

Geographic entities mentioned:
surface_form: st john's in the vale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.593
lon: -3.06
The view north from the vale is dominated by the mountains Blencathra and Skiddaw. High on the western side of the vale lies St John’s in the Vale Church, located in a low pass between High Rigg on the southern side and Low Rigg to the north. This pass provides access for suitably capable vehicles between the vale and Dale Bottom in the Naddle Valley to the west of High Rigg.

Geographic entities mentioned:
surface_form: low rigg
instance_of: Mountain
countries: United Kingdom