Sarmila/GeoWiki-Features huggingface dataset:
J.-C., the Golasecca culture, a Celtic civilization of the Iron Age developed. The latter was in turn conquered by the Romans, who called the lake &quot;Verbanus Lacus&quot; or &quot;Lacus Maximus&quot;. In Roman times a maritime line was created that linked the lake, thanks to Ticino, to Pavia, from where the ships would then continue along the Po to the Adriatic Sea.

Geographic entities mentioned:
surface_form: verbanus lacus
instance_of: Lake
countries: Switzerland
Italy
coordinates: lat: 46.098055555555554
lon: 8.714722222222223
The highest mountain overlooking Lake Maggiore is Monte Rosa (), about west of it. The western bank is in Piedmont (provinces of Novara and Province of Verbano-Cusio-Ossola) and the eastern in Lombardy (province of Varese), whereas the most northerly section extends into the canton of Ticino, where it constitutes its lowest point above sea level as well as that of Switzerland.

Geographic entities mentioned:
surface_form: verbano
instance_of: Lake
countries: Switzerland
Italy
coordinates: lat: 46.098055555555554
lon: 8.714722222222223
The rivers Verzasca, Giona, and Cannobino also flow into the lake. Its outlet is the Ticino which, in turn, joins the river Po just south-east of Pavia. The lake's jagged banks are surrounded by the Pennine and Lepontine Alps, and Lugano Prealps. Prominent peaks around the lake are the Gridone, Monte Tamaro, Monte Nudo and the Mottarone.

Geographic entities mentioned:
surface_form: lugano
instance_of: Lake
countries: Switzerland
Italy
coordinates: lat: 46
lon: 9
Empakaai is nearly always blanketed in mist due to its high altitude, and the lake appears emerald or deep blue in color. The crater is part of the Crater Highlands geographic zone. The rim of the crater offers views of Oldoinyo Lengai, Mount Kilimanjaro, and the Great Rift Valley. Hiking tourism is allowed down the crater. The rim of the crater has two campsites.

Geographic entities mentioned:
surface_form: Oldoinyo Lengai
instance_of: Mountain
countries: Tanzania
coordinates: lat: -2.7616666666667
lon: 35.913333333333
Monte Semprevisa. Monte Semprevisa is the highest peak in the Monti Lepini, in southern Lazio, central Italy. It has an elevation of. It is located across the boundary of the provinces of Rome and Latina, in the territories of Carpineto Romano and Bassiano. Like most of the Lepini peaks, it is composed of limestone rocks.

Geographic entities mentioned:
surface_form: monte semprevisa
instance_of: Mountain
countries: Italy
coordinates: lat: 41.569918
lon: 13.091769
surface_form: semprevisa
instance_of: Mountain
countries: Italy
coordinates: lat: 41.569918
lon: 13.091769
Geography and Demographics. Prazon is located in the Northern District of Israel, in the Gilboa Regional Council jurisdiction. It lies in the Ta'anakh region, a cluster of agricultural villages south of Afula in the Yizre'el Valley area. West of the village runs the seasonal stream Nahal Gilboa, and the surrounding landscape is characterized by fertile farmland of the Yizre'el Valley.

Geographic entities mentioned:
surface_form: Yizre'el Valley
instance_of: Valley
countries: Israel
coordinates: lat: 32.596388888889
lon: 35.241944444444
Mount Dampier. Mount Dampier (&quot;Rakiroa&quot; in Māori) is New Zealand's third highest mountain, rising to. It is located in the Southern Alps, between Mount Hicks and Mount Cook. It is often traversed by climbers en route to the North ridge of Mount Cook. Its Māori name literally means 'long sky' (rangi: sky; roa: long).

Geographic entities mentioned:
surface_form: Mount Cook
instance_of: Mountain
countries: New Zealand
coordinates: lat: -43.595
lon: 170.14194444444445
surface_form: mount hicks
instance_of: Mountain
countries: New Zealand
coordinates: lat: -43.587718
lon: 170.12882
surface_form: mount cook
instance_of: Mountain
countries: New Zealand
coordinates: lat: -43.595
lon: 170.14194444444445
Mount Dampier. Mount Dampier (&quot;Rakiroa&quot; in Māori) is New Zealand's third highest mountain, rising to. It is located in the Southern Alps, between Mount Hicks and Mount Cook. It is often traversed by climbers en route to the North ridge of Mount Cook. Its Māori name literally means 'long sky' (rangi: sky; roa: long).

Geographic entities mentioned:
surface_form: mount dampier
instance_of: Mountain
countries: New Zealand
coordinates: lat: -43.589
lon: 170.14
Mount Dampier. Mount Dampier (&quot;Rakiroa&quot; in Māori) is New Zealand's third highest mountain, rising to. It is located in the Southern Alps, between Mount Hicks and Mount Cook. It is often traversed by climbers en route to the North ridge of Mount Cook. Its Māori name literally means 'long sky' (rangi: sky; roa: long).

Geographic entities mentioned:
surface_form: mount dampier
instance_of: Mountain
countries: New Zealand
coordinates: lat: -43.589
lon: 170.14
surface_form: rakiroa
instance_of: Mountain
countries: New Zealand
coordinates: lat: -43.589
lon: 170.14
Mount Dampier. Mount Dampier (&quot;Rakiroa&quot; in Māori) is New Zealand's third highest mountain, rising to. It is located in the Southern Alps, between Mount Hicks and Mount Cook. It is often traversed by climbers en route to the North ridge of Mount Cook. Its Māori name literally means 'long sky' (rangi: sky; roa: long).

Geographic entities mentioned:
surface_form: mount cook
instance_of: Mountain
countries: New Zealand
coordinates: lat: -43.595
lon: 170.14194444444445
It is located in the Southern Alps, between Mount Hicks and Mount Cook. It is often traversed by climbers en route to the North ridge of Mount Cook. Its Māori name literally means 'long sky' (rangi: sky; roa: long). The English name was originally Mount Hector, after James Hector, but in Fitzgerald's map of 1896 the peak had been renamed after William Dampier.

Geographic entities mentioned:
surface_form: mount hector
instance_of: Mountain
countries: New Zealand
coordinates: lat: -40.952
lon: 175.282
Cumbria. In Cumbria, the ceremony was revived in Warcop and Musgrave at the wish of Septimus Collinson, Provost of Queen's College, Oxford and a native of the village, after being extinct for about thirty years, but an attempt to revive it at Great Langdale proved unsuccessful. Grasmere. At Grasmere the rushbearing took a different form.

Geographic entities mentioned:
surface_form: Great Langdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.449119444444
lon: -3.0733305555556
The property, which is filled with folk art created by artist Mary Nohl (1914–2001), is listed on the National Register of Historic Places. Mary's father Leo, a Milwaukee attorney, and his wife Emma bought the lot along Lake Michigan in 1924, and the family enjoyed summers there in a prefab cottage through the 1920s.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Setting. The Lost Hills Field underlies a long, low range of southeast-to-northwest trending hills of the same name adjacent to the San Joaquin Valley. The hills rise scarcely more than above the San Joaquin Valley to the east, and only or less above the Antelope Plain to the west; in places they are almost flat.

Geographic entities mentioned:
surface_form: San Joaquin Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.628888888889
lon: -120.185
In 1834 the Mexican government granted San Diego the status of a pueblo or chartered town; however, its pueblo status was revoked in 1838 due to declining population. One problem limiting the town's growth was its location far from navigable water. All imports and exports had to be brought ashore in Point Loma and carried several miles over La Playa Trail to the town.

Geographic entities mentioned:
surface_form: Point Loma
instance_of: Landform
countries: United States
coordinates: lat: 32.67
lon: -117.24194444
Extensions of three major mountain chains are located within Serbia proper: Dinaric Alps in the west and south, and the Carpathians and Balkan Mountains in the east. Some notable geographical regions located in central Serbia are: Šumadija, Southern Serbia, Mačva, the Timok Valley (including the Negotin Valley), Pomoravlje, Podunavlje, Posavina, Podrinje, Zlatibor, and Raška. History.

Geographic entities mentioned:
surface_form: Posavina
instance_of: Valley
countries: Croatia
Bosnia and Herzegovina
Serbia
coordinates: lat: 45.16667
lon: 17.33333
Taylor Hills. The Taylor Hills, elevation, is a set of hills southeast of Ekalaka, Montana, in Carter County, Montana.

Geographic entities mentioned:
surface_form: taylor hills
instance_of: Landform
countries: United States
coordinates: lat: 45.65472
lon: -104.46301
Cause of conflict. Tribal rivalry and fighting over cattle has been cited as the primary cause of the conflict. November. In November 2012 over 40 Kenya Police officers and reservists were killed in the Suguta Valley near Baragoi while on a mission to recover stolen cattle. December. Four people were killed and several others injured in renewed cattle raids.

Geographic entities mentioned:
surface_form: Suguta Valley
instance_of: Valley
countries: Kenya
coordinates: lat: 2.0910583333333
lon: 36.513747222222
It lies entirely within the territory of the municipality of Saint-Michel-du-Squatec parish and within Lac-Témiscouata National Park. The mountain is particularly visible from Lake Témiscouata, which forms a right angle with the mountain, as well as from Cabano, just three kilometers from the summit. Topography.

Geographic entities mentioned:
surface_form: Lake Témiscouata
instance_of: Lake
countries: Canada
coordinates: lat: 47.666666666667
lon: -68.833333333333
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: lake témiscouata
instance_of: Lake
countries: Canada
coordinates: lat: 47.666666666667
lon: -68.833333333333
They are aligned on a southwest–northeast axis, corresponding to the major Appalachian folding axes. The altitude of these peaks varies from 300 to 380 m, culminating in Montagne du Fourneau and an unnamed summit near Lac Aubert. Montagne du Fourneau is bordered by a 170 m escarpment in contact with Lake Témiscouata. Geology.

Geographic entities mentioned:
surface_form: Lake Témiscouata
instance_of: Lake
countries: Canada
coordinates: lat: 47.666666666667
lon: -68.833333333333
surface_form: lake témiscouata
instance_of: Lake
countries: Canada
coordinates: lat: 47.666666666667
lon: -68.833333333333
Fauna and flora. The Témiscouata region is home to 40 species of mammals, 20 of which are found in the park. The most common species are white-tailed deer, moose, snowshoe hare, pine marten, american mink, red fox, coyote, and muskrat. The mountain is entirely included in the Lake Témiscouata white-tailed deer overwintering, the largest in the Lower St. Lawrence region.

Geographic entities mentioned:
surface_form: Lake Témiscouata
instance_of: Lake
countries: Canada
coordinates: lat: 47.666666666667
lon: -68.833333333333
surface_form: lake témiscouata
instance_of: Lake
countries: Canada
coordinates: lat: 47.666666666667
lon: -68.833333333333
History. The oldest traces of human occupation in the region date from 9,000 to 9,400 years BC at a Paleoindian archaeological site a few kilometers north of Saint-Michel-du-Squatec. Located on a major traffic route linking the Bay of Fundy to the St. Lawrence River, Lake Témiscouata was known to at least four Amerindian groups: the Maliseet, the Mi'kmaq, the Montagnais and the St.

Geographic entities mentioned:
surface_form: Lake Témiscouata
instance_of: Lake
countries: Canada
coordinates: lat: 47.666666666667
lon: -68.833333333333
surface_form: lake témiscouata
instance_of: Lake
countries: Canada
coordinates: lat: 47.666666666667
lon: -68.833333333333
Lawrence Iroquoians. 1,000 years ago, the region was occupied by the Maliseet. Archaeological research shows that the region was frequented on a seasonal basis by highly mobile populations. In the Late Woodland period, between 500 and 1,000 years BC, archaeological evidence suggests that Lake Témiscouata populations maintained trade links with the St. Lawrence Valley and the Bay of Fundy.

Geographic entities mentioned:
surface_form: Lake Témiscouata
instance_of: Lake
countries: Canada
coordinates: lat: 47.666666666667
lon: -68.833333333333
surface_form: lake témiscouata
instance_of: Lake
countries: Canada
coordinates: lat: 47.666666666667
lon: -68.833333333333
surface_form: lake témiscouata
instance_of: Lake
countries: Canada
coordinates: lat: 47.666666666667
lon: -68.833333333333
Lawrence Valley and the Bay of Fundy. The existence of Lake Témiscouata was known to the first French settlers in North America. Samuel de Champlain was informed of the lake's presence as early as 1604, before the founding of Quebec in 1608. The first water route between the St. Lawrence and St.

Geographic entities mentioned:
surface_form: Lake Témiscouata
instance_of: Lake
countries: Canada
coordinates: lat: 47.666666666667
lon: -68.833333333333
Starting in 1996, the government undertook studies to identify potential park sites in the southern part of the province. In the case of the Notre-Dame Mountains, seven sites were analyzed, including Lake Témiscouata. A comparative analysis combined with an aerial survey determined that it was the most representative of its natural region.

Geographic entities mentioned:
surface_form: Lake Témiscouata
instance_of: Lake
countries: Canada
coordinates: lat: 47.666666666667
lon: -68.833333333333
surface_form: lake témiscouata
instance_of: Lake
countries: Canada
coordinates: lat: 47.666666666667
lon: -68.833333333333
Montagne du Fourneau. Montagne du Fourneau is a mountain in the Lac-Témiscouata National Park in Quebec, Canada. It owes its name to the fact that during the first half of the 19th century, the mountain's limestone deposits were used to fuel a lime kiln at Fort Ingall. It was then used as forest land by the owners of the Madawaska Seignory.

Geographic entities mentioned:
surface_form: montagne du fourneau
instance_of: Mountain
countries: Canada
coordinates: lat: 47.70944
lon: -68.86833
Montagne du Fourneau. Montagne du Fourneau is a mountain in the Lac-Témiscouata National Park in Quebec, Canada. It owes its name to the fact that during the first half of the 19th century, the mountain's limestone deposits were used to fuel a lime kiln at Fort Ingall. It was then used as forest land by the owners of the Madawaska Seignory.

Geographic entities mentioned:
surface_form: montagne du fourneau
instance_of: Mountain
countries: Canada
coordinates: lat: 47.70944
lon: -68.86833
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
When Fort Ingall was built in 1839, the British used the mountain's limestone to make lime. They used it to make mortar and whitewash the interior and exterior of buildings. The mountain has also been known as &quot;Mount Lennox&quot;, &quot;Mount Wisik&quot; and &quot;Furnace Mountain&quot;. Location.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
They are aligned on a southwest–northeast axis, corresponding to the major Appalachian folding axes. The altitude of these peaks varies from 300 to 380 m, culminating in Montagne du Fourneau and an unnamed summit near Lac Aubert. Montagne du Fourneau is bordered by a 170 m escarpment in contact with Lake Témiscouata. Geology.

Geographic entities mentioned:
surface_form: montagne du fourneau
instance_of: Mountain
countries: Canada
coordinates: lat: 47.70944
lon: -68.86833
surface_form: montagne du fourneau
instance_of: Mountain
countries: Canada
coordinates: lat: 47.70944
lon: -68.86833
Weather. According to Litynski's numerical classification of world climates, the climate on Montagne du Fourneau is subpolar, subhumid, intermediate continental, with insolation below the global average. According to the Notre-Dame-du-Lac weather station (320 m), between 1981 and 2010, the average annual temperature was 3.2 °C, with an average of -13.7 °C in January and 17.9 °C in July.

Geographic entities mentioned:
surface_form: montagne du fourneau
instance_of: Mountain
countries: Canada
coordinates: lat: 47.70944
lon: -68.86833
This trail allows viewers to explore the pine forest, classified as an exceptional forest ecosystem, and offers views of the lake and Cabano. The mountain is also on the route of a long-distance hiking trail, the Montagne du Fourneau section of the national trail, whose Bas-Saint-Laurent section links Trois-Pistoles to Dégelis via the national park.

Geographic entities mentioned:
surface_form: montagne du fourneau
instance_of: Mountain
countries: Canada
coordinates: lat: 47.70944
lon: -68.86833
This formation is part of the Gaspé belt, which comprises rocks from the same periods that were deformed and metamorphosed during the Acadian orogeny some 400 million years ago. Together with the Robitaille and Lac Croche formations, it also constitutes the Squatec-Cabano syncline. This is delimited to the east and west by two thrust faults that separate the mountain from the older rocks.

Geographic entities mentioned:
surface_form: lac croche
instance_of: Lake
countries: Canada
coordinates: lat: 46.831943055555556
lon: -72.5
surface_form: lac croche
instance_of: Lake
countries: Canada
coordinates: lat: 52.6667
lon: -105.583
Montagne du Fourneau. Montagne du Fourneau is a mountain in the Lac-Témiscouata National Park in Quebec, Canada. It owes its name to the fact that during the first half of the 19th century, the mountain's limestone deposits were used to fuel a lime kiln at Fort Ingall. It was then used as forest land by the owners of the Madawaska Seignory.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
The unconceded lands of the seigneury were acquired by the Quebec government in 1969. The mountain is home to a red pine-white pine forest, a forest group that was classified as an exceptional forest ecosystem in 2003 due to its rarity in Eastern Quebec. This rarity is attributable to the low number of forest fires in the region, due to its high humidity.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Lawrence. It was included in the Lac-Témiscouata National Park when it was created back in 2009. Toponymy. Kiln Mountain probably owes its name to the presence of a kiln for converting limestone into lime, which was located near Fort Ingall on the opposite shore of the lake. When Fort Ingall was built in 1839, the British used the mountain's limestone to make lime.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Toponymy. Kiln Mountain probably owes its name to the presence of a kiln for converting limestone into lime, which was located near Fort Ingall on the opposite shore of the lake. When Fort Ingall was built in 1839, the British used the mountain's limestone to make lime. They used it to make mortar and whitewash the interior and exterior of buildings.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Together with the Robitaille and Lac Croche formations, it also constitutes the Squatec-Cabano syncline. This is delimited to the east and west by two thrust faults that separate the mountain from the older rocks. The positive relief of the syncline is mainly explained by the fact that it is composed of rocks that are more resistant than the surrounding ones.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
The region enjoys an average frost-free season of 122 days. Precipitation in the region is comparable to that of the Notre-Dame Mountains and the south shore of the St. Lawrence River, but it is one of the regions with the lowest annual snowfall in southern Quebec. Average annual insolation is 1,706 hours, a deficit of 348 hours compared to Montreal.

Geographic entities mentioned:
surface_form: montreal
instance_of: Lake
countries: Canada
coordinates: lat: 54.3333
lon: -105.667
Fauna and flora. The Témiscouata region is home to 40 species of mammals, 20 of which are found in the park. The most common species are white-tailed deer, moose, snowshoe hare, pine marten, american mink, red fox, coyote, and muskrat. The mountain is entirely included in the Lake Témiscouata white-tailed deer overwintering, the largest in the Lower St. Lawrence region.

Geographic entities mentioned:
surface_form: moose
instance_of: Watercourse
countries: Canada
coordinates: lat: 52.91444444444444
lon: -118.80638888888889
The fir should eventually regain its place as it dominates regeneration. To the south of the mountain is a sugar maple grove. On the steep western and south-western slopes of the mountain is a red pine-white pine forest, exceptional both for its rarity in eastern Quebec and for its size (207 ha). This is the result of repeated forest fires in this area.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
The mountain's escarpment and scree slopes are home to the region's only occurrence of a few species: Ivory sedge, Steller's rockbrake, Northern wild comfrey (&quot;Cynoglossum virginianum var. boreale&quot;), Fragrant woodfern, Jack pine, bog-rosemary, mountain cranberry, oblong woodsia and Glabrous woodsia. History.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
As a result, the entire eastern part of the lake, with the exception of Saint-Juste-du-Lac, remains untouched by human occupation. Forest exploitation along the Vieille Route (south of the mountain) began in the late 19th century. Lumber camps were set up every two, six, and twelve miles from the Lake Témiscouasta wharf. Each winter, these camps could hold up to a hundred men.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Since 2003, the mountain's western flank has also been protected by the Montagne-à-Fourneau rare forest, an exceptional 207-hectare forest ecosystem, with the aim of protecting a forest of red pines accompanied by white pines, a very rare forest stand in eastern Quebec made possible by high humidity and an absence of forest fires.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
The southeastern part of the mountain is also part of a 394.2 ha biological refuge created in 2003 to protect old-growth forests from the forestry industry. Hiking. The summit of the mountain is accessible via the Montagne-du-Fourneau trail, a 5.5 km-long loop that begins at the national park's discovery and service center.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
This is the result of repeated forest fires in this area. It is currently dominated by red pines reaching 18 m in height and 32 cm in diameter. Its origins date back to a fire around 1860. Red pine is accompanied by white pine, black spruce, balsam fir, eastern white-cedar, balsam poplar, and white birch. The shrub layer is composed of Eagle Fern, Lingonberry, and umbellate wintergreen.

Geographic entities mentioned:
surface_form: cedar
instance_of: Lake
countries: Canada
coordinates: lat: 53.366666666667
lon: -100
Isku. Isku (Quechua for lime, hispanicized spelling &quot;Iscu&quot;) is a mountain in the Andes of Peru, about high. It is located in the Lima Region, Oyón Province, Oyón District. Isku lies southeast of Yana Uqhu.

Geographic entities mentioned:
surface_form: uqhu
instance_of: Mountain
countries: Peru
coordinates: lat: -11.7878
lon: -76.0631
surface_form: yana uqhu
instance_of: Mountain
countries: Peru
coordinates: lat: -14.5975
lon: -72.8361
surface_form: uqhu
instance_of: Mountain
countries: Peru
coordinates: lat: -11.8958
lon: -76.2414
surface_form: yana uqhu
instance_of: Mountain
countries: Peru
coordinates: lat: -10.6067
lon: -76.7264
surface_form: yana uqhu
instance_of: Mountain
countries: Peru
coordinates: lat: -11.05222222
lon: -76.66666667
surface_form: uqhu
instance_of: Mountain
countries: Peru
coordinates: lat: -11.5225
lon: -76.2464
Isku. Isku (Quechua for lime, hispanicized spelling &quot;Iscu&quot;) is a mountain in the Andes of Peru, about high. It is located in the Lima Region, Oyón Province, Oyón District. Isku lies southeast of Yana Uqhu.

Geographic entities mentioned:
surface_form: isku
instance_of: Mountain
countries: Peru
coordinates: lat: -10.61444444
lon: -76.70722222
Route description. State Route 373 begins at the California state line, approximately north of the town of Death Valley Junction, California on California SR 127. The highway heads almost due north from this location, passing through the Amargosa Valley. On the west side of the highway, the farm lands and homes of the community of Amargosa Valley come into view.

Geographic entities mentioned:
surface_form: Amargosa Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.6333
lon: -116.4
Wila Qullu (Ingavi). Wila Qullu (Aymara &quot;wila&quot; blood, blood-red, &quot;qullu&quot; mountain, &quot;red mountain&quot;) is a mountain in the Chilla-Kimsa Chata mountain range in the Andes of Bolivia which reaches a height of approximately. It is located in the La Paz Department, Ingavi Province, on the border of the municipalities of Jesús de Machaca and Tiwanaku.

Geographic entities mentioned:
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.3833
lon: -68.9667
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.51361111
lon: -66.96194444
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -20.3333
lon: -68.65
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.37833333
lon: -66.68833333
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.0833
lon: -66.3333
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.9719
lon: -66.3703
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.12694444
lon: -68.27916667
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.7833
lon: -68.8333
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -20.97472222
lon: -66.38083333
surface_form: wila qullu (ingavi)
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.67472222
lon: -68.625
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.2953
lon: -69.3989
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.065
lon: -66.3222
Wila Qullu (Ingavi). Wila Qullu (Aymara &quot;wila&quot; blood, blood-red, &quot;qullu&quot; mountain, &quot;red mountain&quot;) is a mountain in the Chilla-Kimsa Chata mountain range in the Andes of Bolivia which reaches a height of approximately. It is located in the La Paz Department, Ingavi Province, on the border of the municipalities of Jesús de Machaca and Tiwanaku.

Geographic entities mentioned:
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.3833
lon: -68.9667
surface_form: kimsa chata
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.1058
lon: -68.3858
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.51361111
lon: -66.96194444
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -20.3333
lon: -68.65
surface_form: kimsa chata
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.1214
lon: -68.3297
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.37833333
lon: -66.68833333
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.0833
lon: -66.3333
surface_form: kimsa chata
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.71666667
lon: -68.7
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.9719
lon: -66.3703
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.12694444
lon: -68.27916667
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.7833
lon: -68.8333
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -20.97472222
lon: -66.38083333
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.67472222
lon: -68.625
surface_form: kimsa chata
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.10972222
lon: -67.66222222
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.2953
lon: -69.3989
surface_form: kimsa chata
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.88333333
lon: -68.85
surface_form: wila qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.065
lon: -66.3222
Mawson Glacier. The Mawson Glacier () is a large glacier on the east coast of Victoria Land, Antarctica, descending eastward from the Antarctic Plateau to the north of Trinity Nunatak and the Kirkwood Range, to enter the Ross Sea, where it forms the Nordenskjöld Ice Tongue.

Geographic entities mentioned:
surface_form: Antarctic Plateau
instance_of: Plateau
coordinates: lat: -90
lon: 0
It flows past Charcot Cove and Bruce Point to the north and the Oates Piedmont Glacier and Cape Day to its south, to terminate in the NordenSkjold Ice Tongue. Battlements Nunatak. A large nunatak near the head of Mawson Glacier, about northwest of Allan Hills. It is mostly ice free and has a number of small peaks running in a line west from the main peak.

Geographic entities mentioned:
surface_form: Allan Hills
instance_of: Landform
coordinates: lat: -76.7
lon: 159.7
Northern Survey Party of the CTAE (1956–58) after Capt. Lawrence E.G. Oates who, with Captain Scott and three companions, perished on the return from the South Pole in 1912. Cape Day. A cape on the coast of Victoria Land east of Mount Gauss. First charted by the BrAE (1907–09) which named this cape after Bernard C. Day, electrician and motor expert with the expedition.

Geographic entities mentioned:
surface_form: Mount Gauss
instance_of: Mountain
coordinates: lat: -76.316666666667
lon: 162.03333333333
William M. Tugman State Park is a state park in the U.S. state of Oregon. Administered by the Oregon Parks and Recreation Department (OPRD), the park borders Eel Lake, about south of Reedsport near U.S. Route 101. Tugman Park has 94 campsites for recreational vehicles (RVs) as well as 16 yurts for hikers and bikers; a day-use area, a boat ramp, a fishing dock, and a hiking trail.

Geographic entities mentioned:
surface_form: Eel Lake
instance_of: Lake
countries: United States
coordinates: lat: 43.6022
lon: -124.175
September 1996 expedition. In the fall of 1996, Lopsang returned to Everest as a guide, working for a Japanese expedition. On 25 September 1996, a large avalanche erupted during the ascent on the southeast ridge route in the area between Camp III at the top of the Lhotse face, and Camp IV at the South Col, the starting point for the final summit push.

Geographic entities mentioned:
surface_form: Lhotse
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.961666666667
lon: 86.933333333333
Rhinodoras thomersoni. &quot;Rhinodoras thomersoni&quot; is a species of thorny catfish native to Colombia and Venezuela where it is found in the river basins along the southwest shore of Lake Maracaibo (Santa Ana, Catatumbo and Escalante Rivers). This species grows to a length of SL.

Geographic entities mentioned:
surface_form: Lake Maracaibo
instance_of: Lake
countries: Venezuela
coordinates: lat: 9.8158333333333
lon: -71.556666666667
Witnesses have been intimidated and even murdered, as in the case of the former police inspector Milan Josipović, shot and killed when he was said to be prepared to give evidence at a trial of high-level officials. Investigators recovering bodies revealed by the draining of Lake Perućac in 2010 continued to encounter a lack of local cooperation.

Geographic entities mentioned:
surface_form: Lake Perućac
instance_of: Lake
countries: Bosnia and Herzegovina
coordinates: lat: 43.965024
lon: 19.410753
As the hurricane approached Northern commercial flights were grounded, and 1,500 National Guard troops were readied to be mobilized if needed by Florida Governor Millard Caldwell. 4,700 persons in Broward County moved into Red Cross shelters, while up to 15,000 people evacuated the flood-prone Lake Okeechobee region. In all, more than 40,000 people statewide moved into Red Cross shelters.

Geographic entities mentioned:
surface_form: Lake Okeechobee
instance_of: Lake
countries: United States
coordinates: lat: 26.933333333333
lon: -80.8
The tornado damaged or destroyed 58 homes over a area, inflicting F3-level damage on the present Fujita scale. Gulf Coast of the United States. Wind instruments at Moisant Field were disabled after recording sustained winds of. Due to northerly winds, water overtopped sections of the levees on Lake Pontchartrain, leaving some lakefront streets &quot;waist deep,&quot; above the delimiter.

Geographic entities mentioned:
surface_form: Lake Pontchartrain
instance_of: Lake
countries: United States
coordinates: lat: 30.188888888889
lon: -90.101388888889
Bazigaba. The Bazigaba or Zigaba clan is a large multi-tribal clan of the great Banyakitara people in the African Great Lakes region. One who belongs to this clan is called Omuzigaba/ Muzigaba/Umuzigaba and the plural is Abazigaba.

Geographic entities mentioned:
surface_form: African Great Lakes
instance_of: Group of lakes
countries: Burundi
Zambia
Kenya
Democratic Republic of the Congo
Malawi
Mozambique
Rwanda
Tanzania
Uganda
Ethiopia
coordinates: lat: -8
lon: 35
According to Bazigaba's oral history, the Bazigaba descend from an eponymous ancestor named Kazigaba who along with his brother Rurenge and their sister Nyirankende originated in Gisaka Northwest Tanzania near Lake Nyanza (Victoria).

Geographic entities mentioned:
surface_form: Victoria
instance_of: Lake
countries: Tanzania
Uganda
Kenya
coordinates: lat: -1
lon: 33
Location and description. The main island is quite mountainous; the only flat area is the location of the capital, Edinburgh of the Seven Seas, on the northwest coast, and of the agricultural area named Potato Patches. The highest point is a volcano called Queen Mary's Peak reaching; it is covered by snow in winter and is listed as an ultra prominent peak.

Geographic entities mentioned:
surface_form: Queen Mary's Peak
instance_of: Mountain
countries: United Kingdom
coordinates: lat: -37.11175
lon: -12.287805555555556
Zhivkov took action against what he saw as a cults of personality – whether in relation to Stalin, Chervenkov or to other figures. Monuments considered as being part of such cults were taken down and many public places renamed – the most prominent of which were the return of &quot;Mount Stalin&quot; back to its prewar name of Mount Musala and that of the city of &quot;Stalin&quot; back to Varna.

Geographic entities mentioned:
surface_form: Musala
instance_of: Mountain
countries: Bulgaria
coordinates: lat: 42.179167
lon: 23.585278
Supported ground forces in Operation Dragoon, the invasion of Southern France and drive northwards though Lyon until linking with Allied ground forces in eastern France. Returned to Italy and engaged enemy forces in the Po Valley, then returning to France in the spring of 1945 and supporting ground forces during the Western Allied invasion of Germany in March/April 1945.

Geographic entities mentioned:
surface_form: Po Valley
instance_of: Valley
countries: Italy
coordinates: lat: 45.330277777778
lon: 9.7988888888889
The coastal areas were low and marshy while the interior of the municipality was mountainous. The highest point in the municipality was the tall mountain Kvannfjellet. Other notable mountains in Fræna were Jendemsfjellet, Høgheitinden, and Lågheiane. The Bjørnsund islands were located off the northwestern coast of Fræna. They are now uninhabited, but the Bjørnsund Lighthouse is still in operation.

Geographic entities mentioned:
surface_form: Jendemsfjellet
instance_of: Mountain
countries: Norway
coordinates: lat: 62.800833333333
lon: 7.0436111111111
surface_form: Høgheitinden
instance_of: Mountain
countries: Norway
coordinates: lat: 62.8737
lon: 7.216
However, its territory also includes most of the small islands surrounding Manitoulin, even those at the far western end of Manitoulin. The town was created on January 1, 1998, by amalgamating the Town of Little Current with the Township of Howland and the unorganized small islands in Lake Huron. It is the administrative headquarters of the Aundeck Omni Kaning First Nations band government.

Geographic entities mentioned:
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
The cold season does not have many differences with other North American places of the same parallel. However, the obvious differing factor is that all weather is dictated by Lake Huron. As such, the lake generates microclimates similar to coastal cities, thousands of miles away; one example is Asahikawa, on the northern Japanese island of Hokkaido. Demographics.

Geographic entities mentioned:
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
It is well marked from the east by Strawberry Island Lighthouse and from the west by a series of navigational markers. The only land access to Manitoulin is the Little Current Swing Bridge, located on Highway 6, crossing the North Channel of Lake Huron to the mainland, where the highway continues northward to Espanola.

Geographic entities mentioned:
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
Pälkänevesi. Pälkänevesi is a lake in Finland. The lake is located in the municipality of Pälkäne in the Pirkanmaa region. The lake is part of Kokemäenjoki basin and a chain of lakes that consists of Längelmävesi, Vesijärvi, Roine, Pälkänevesi and Mallasvesi.

Geographic entities mentioned:
surface_form: Längelmävesi
instance_of: Lake
countries: Finland
coordinates: lat: 61.53526
lon: 24.37048
surface_form: Mallasvesi
instance_of: Lake
countries: Finland
coordinates: lat: 61.3
lon: 24.15
surface_form: pälkänevesi
instance_of: Lake
countries: Finland
coordinates: lat: 61.36666667
lon: 24.36666667
surface_form: vesijärvi
instance_of: Lake
countries: Finland
coordinates: lat: 61.50205
lon: 24.10458
The lake is part of Kokemäenjoki basin and a chain of lakes that consists of Längelmävesi, Vesijärvi, Roine, Pälkänevesi and Mallasvesi. This chain of lakes drains into Vanajavesi in Valkeakoski and from southeast another chain of lakes, consisting of the lakes Lummene, Kuohijärvi, Kukkia, Iso-Roine, Hauhonselkä and Ilmoilanselkä joins into it.

Geographic entities mentioned:
surface_form: Vanajavesi
instance_of: Lake
countries: Finland
coordinates: lat: 61.16666667
lon: 24.25
surface_form: Lummene
instance_of: Lake
countries: Finland
coordinates: lat: 61.48333333
lon: 25.05
surface_form: Kuohijärvi
instance_of: Lake
countries: Finland
coordinates: lat: 61.22395
lon: 24.89048
surface_form: Kukkia
instance_of: Lake
countries: Finland
coordinates: lat: 61.33818
lon: 24.70639
surface_form: Iso-Roine
instance_of: Lake
countries: Finland
coordinates: lat: 61.2175
lon: 24.56713
surface_form: Hauhonselkä
instance_of: Lake
countries: Finland
coordinates: lat: 61.16587
lon: 24.51301
surface_form: Ilmoilanselkä
instance_of: Lake
countries: Finland
coordinates: lat: 61.21945
lon: 24.41611
Pälkänevesi. Pälkänevesi is a lake in Finland. The lake is located in the municipality of Pälkäne in the Pirkanmaa region. The lake is part of Kokemäenjoki basin and a chain of lakes that consists of Längelmävesi, Vesijärvi, Roine, Pälkänevesi and Mallasvesi.

Geographic entities mentioned:
surface_form: pälkänevesi
instance_of: Lake
countries: Finland
coordinates: lat: 61.36666667
lon: 24.36666667
Sanchez Reservoir. Sanchez Reservoir lies in far southcentral Colorado, west of the Sangre de Cristo Mountains in Costilla County. Its inflows include Ventero Creek and the Sanchez Canal, a diversion canal that takes water from Culebra Creek and two other creeks. Dam. The reservoir's earthen dam was built in 1912.

Geographic entities mentioned:
surface_form: sanchez reservoir
instance_of: Body of water
countries: United States
coordinates: lat: 37.08388889
lon: -105.41444444
Fishing. Colorado Parks and Wildlife manages fishing at the reservoir, which forms the Sanchez Reservoir State Wildlife Area. However, the Colorado Department of Public Health and Environment has issued a &quot;Fish consumption advisory,&quot; warning of unsafe mercury levels in northern pike and walleye caught in the lake.

Geographic entities mentioned:
surface_form: sanchez reservoir
instance_of: Body of water
countries: United States
coordinates: lat: 37.08388889
lon: -105.41444444
Death and contemporary assessment. While on patrol in Walvis Bay he was mortally wounded and died shortly afterwards on 21 January 1915, aged 42, one of the first victims of the campaign in South West Africa. Dr Marloth, in his obituary for the Mountain Club Journal, mentions the last delivery he received from Dyke: 50 species of plants collected during a week of camping on Mont-Aux-Sources.

Geographic entities mentioned:
surface_form: Mont-Aux-Sources
instance_of: Mountain
countries: Lesotho
South Africa
coordinates: lat: -28.759080555556
lon: 28.884644444444
Beyşehir gudgeon. The Beyşehir gudgeon (&quot;Gobio microlepidotus&quot;) is a species of gudgeon, a small freshwater ray-finned fish in the family Gobionidae. It is endemic to Lake Beyşehir in Turkey.

Geographic entities mentioned:
surface_form: Lake Beyşehir
instance_of: Lake
countries: Turkey
coordinates: lat: 37.782
lon: 31.5076
Rijpdalen. Rijpdalen is a valley in the central part of Nordaustlandet, Svalbard, separating Gustav V Land from Prins Oscars Land. The valley extends between the head of Wahlenbergfjorden and the head of Rijpfjorden. The valley is named after Dutch explorer Jan Rijp. At the watershed in Rijpdalen is the plain of Helvetesflya.

Geographic entities mentioned:
surface_form: rijpdalen
instance_of: Valley
countries: Norway
coordinates: lat: 79.919166666667
lon: 22.251944444444
The valley extends between the head of Wahlenbergfjorden and the head of Rijpfjorden. The valley is named after Dutch explorer Jan Rijp. At the watershed in Rijpdalen is the plain of Helvetesflya. The ice caps of Vestfonna and Austfonna are separated by Rijpdalen and Helvetesflya.

Geographic entities mentioned:
surface_form: rijpdalen
instance_of: Valley
countries: Norway
coordinates: lat: 79.919166666667
lon: 22.251944444444
They spent spring and summer inland, where they intercepted caribou travelling north in the spring, and camped in summer on the calving grounds.&quot;
These inland Inuit also lived along the banks of the Kazan River, Little Dubawnt Lake (renamed Kamilikuak) and north of Thlewiaza (&quot;Big River&quot;)
The Ihalmiut were successful inland hunters.

Geographic entities mentioned:
surface_form: Dubawnt Lake
instance_of: Lake
countries: Canada
coordinates: lat: 63.1
lon: -101.53333333333
surface_form: kamilikuak
instance_of: Lake
countries: Canada
coordinates: lat: 63.1
lon: -101.53333333333
surface_form: dubawnt lake
instance_of: Lake
countries: Canada
coordinates: lat: 63.1
lon: -101.53333333333
The plane departed Points North Landing, Saskatchewan with of cargo on board for building materials for the construction of a lodge. Relocations. The Ihalmiut were relocated by the Government of Canada in May 1957 to Henik Lake. The caribou were scarce in the Henik Lake area and starvation soon set in. They were later relocated again to Whale Cove.

Geographic entities mentioned:
surface_form: Henik Lake
instance_of: Group of lakes
countries: Canada
coordinates: lat: 61.64982
lon: -97.54021
surface_form: henik lake
instance_of: Group of lakes
countries: Canada
coordinates: lat: 61.64982
lon: -97.54021
Fauna. Ennadai Lake is part of the &quot;annual migration route of the almost 500,000 strong Qamanirjuaq barren-ground caribou herd, and the occasional route of the 275,000 member Beverly herd.&quot; Beverly Lake is the area where the Beverly herd regularly bears its young. The Qamanirjuaq herd regularly bears its young near Qamanirjuaq Lake.

Geographic entities mentioned:
surface_form: Qamanirjuaq Lake
instance_of: Lake
countries: Canada
coordinates: lat: 62.983333333333
lon: -96.566666666667
Ennadai Lake. Ennadai Lake is a lake in the Kivalliq Region, Nunavut, Canada. It is long, and wide. It is drained to the north by the Kazan River. A section of the Kazan River from the outlet of Ennadai Lake to Baker Lake, was designated as a part of the Canadian Heritage Rivers System in 1990. A weather station was located in the area at Ennadai. History.

Geographic entities mentioned:
surface_form: ennadai lake
instance_of: Lake
countries: Canada
coordinates: lat: 60.96666667
lon: -101.33305556
Ennadai Lake. Ennadai Lake is a lake in the Kivalliq Region, Nunavut, Canada. It is long, and wide. It is drained to the north by the Kazan River. A section of the Kazan River from the outlet of Ennadai Lake to Baker Lake, was designated as a part of the Canadian Heritage Rivers System in 1990. A weather station was located in the area at Ennadai. History.

Geographic entities mentioned:
surface_form: ennadai lake
instance_of: Lake
countries: Canada
coordinates: lat: 60.96666667
lon: -101.33305556
surface_form: baker lake
instance_of: Lake
countries: Canada
coordinates: lat: 64.16666666666667
lon: -95.5
It is long, and wide. It is drained to the north by the Kazan River. A section of the Kazan River from the outlet of Ennadai Lake to Baker Lake, was designated as a part of the Canadian Heritage Rivers System in 1990. A weather station was located in the area at Ennadai. History. Until 1957, Ennadai Lake was home to the Ahiarmiut (Ihalmiut) Inuktitut syllabics ᐃᐦᐊᓪᒥᐅᑦ, Caribou Inuit.

Geographic entities mentioned:
surface_form: ennadai
instance_of: Lake
countries: Canada
coordinates: lat: 60.96666667
lon: -101.33305556
A weather station was located in the area at Ennadai. History. Until 1957, Ennadai Lake was home to the Ahiarmiut (Ihalmiut) Inuktitut syllabics ᐃᐦᐊᓪᒥᐅᑦ, Caribou Inuit. Inland Inuit were also &quot;known as the (&quot;People from Beyond&quot;) or Ahiarmiut (&quot;the Out-of-the-Way Dwellers&quot;).

Geographic entities mentioned:
surface_form: ennadai lake
instance_of: Lake
countries: Canada
coordinates: lat: 60.96666667
lon: -101.33305556
Caribou meat was dried for the winter months. On March 17, 2000, two pilots perished in an aviation accident while landing a Douglas DC-3 at Ennadai Lake. The plane departed Points North Landing, Saskatchewan with of cargo on board for building materials for the construction of a lodge. Relocations. The Ihalmiut were relocated by the Government of Canada in May 1957 to Henik Lake.

Geographic entities mentioned:
surface_form: ennadai lake
instance_of: Lake
countries: Canada
coordinates: lat: 60.96666667
lon: -101.33305556
They were later relocated again to Whale Cove. The relocations to Nueltin Lake and Henik Lake were complete failures. &quot;The Ahiarmiut themselves maintain that Ennadai Lake was an excellent hunting area and failed to understand why they were relocated.&quot;
On September 7, 1985, 36 elders returned to Ennadai Lake from where they had been relocated in the 1950s.

Geographic entities mentioned:
surface_form: ennadai lake
instance_of: Lake
countries: Canada
coordinates: lat: 60.96666667
lon: -101.33305556