Sarmila/GeoWiki-Features huggingface dataset:
It is in Big Lakes County and Municipal District of Smoky River No. 130, northeast of the junction of Highway 2 and Highway 679. It lies in the hydrographic basin of the Athabasca River. The name comes from a Cree phrase meaning &quot;dirty-water lake&quot;: (). The lake contains lake whitefish, yellow perch, northern pike and walleye.

Geographic entities mentioned:
surface_form: athabasca
instance_of: Lake
countries: Canada
coordinates: lat: 59.266666666667
lon: -109.45
surface_form: athabasca
instance_of: Mountain
countries: Canada
coordinates: lat: 52.18055555555556
lon: -117.20166666666667
Winagami Lake. Winagami Lake () is a large and shallow lake in northern Alberta, Canada. It is in Big Lakes County and Municipal District of Smoky River No. 130, northeast of the junction of Highway 2 and Highway 679. It lies in the hydrographic basin of the Athabasca River. The name comes from a Cree phrase meaning &quot;dirty-water lake&quot;: ().

Geographic entities mentioned:
surface_form: winagami lake
instance_of: Lake
countries: Canada
coordinates: lat: 55.6456
lon: -116.77
The village, in the municipality of Nea Propontida, is built on a hill overlooking the Thermaikos Gulf. Most of the village is only a few minutes from the sea, and on a clear day, there is a wonderful view across the bay to Mount Olympus. Flogita was founded in 1923, when refugees fleeing from Anatolia after the Greco-Turkish War assembled to build New (Nea) Flogita.

Geographic entities mentioned:
surface_form: Mount Olympus
instance_of: Mountain
countries: Greece
coordinates: lat: 40.083333333333336
lon: 22.35
Early in the 16th century, Muhammad al-Fasi established the Awlad Muhammad dynasty of Murzuq, which would hold power in the city until 1812. Al-Fasi is traditionally held to be a Moroccan sharif, but according to John Ralph Willis, oral tradition indicates that he was a pilgrim from Saguia el-Hamra in present-day Western Sahara.

Geographic entities mentioned:
surface_form: Saguia el-Hamra
instance_of: Valley
countries: Western Sahara
Morocco
coordinates: lat: 27.1536
lon: -13.2033
Volcanism of the Mount Edziza volcanic complex. The Mount Edziza volcanic complex (MEVC) in British Columbia, Canada, has a history of volcanism that spans more than 7 million years. It has taken place during five cycles of magmatic activity, each producing less volcanic material than the previous one.

Geographic entities mentioned:
surface_form: Mount Edziza volcanic complex
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5
lon: -130.6
Background. The Mount Edziza volcanic complex is a linear group of volcanoes in northwestern British Columbia, Canada. It is about long and wide, consisting of several stratovolcanoes, shield volcanoes, subglacial volcanoes, lava domes and cinder cones. This volcanic complex includes a broad, steep-sided, intermontane plateau that rises from a base elevation of.

Geographic entities mentioned:
surface_form: Mount Edziza volcanic complex
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5
lon: -130.6
A northerly-trending, elliptical, shield volcano consisting of multiple flat-lying lava flows forms the plateau which is capped with several smaller volcanic structures of the complex. Four central volcanoes of felsic composition overlie the plateau, the highest of which is Mount Edziza with an elevation of.

Geographic entities mentioned:
surface_form: Mount Edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
Four central volcanoes of felsic composition overlie the plateau, the highest of which is Mount Edziza with an elevation of. The plateau is subdivided into three smaller plateaus; from north to south they are the Big Raven, Kitsu and Arctic Lake plateaus. The MEVC is one of the largest volcanic complexes in North America, covering about and comprising about of volcanic material.

Geographic entities mentioned:
surface_form: Big Raven
instance_of: Plateau
countries: Canada
coordinates: lat: 57.7167
lon: -130.75
surface_form: Kitsu
instance_of: Plateau
countries: Canada
coordinates: lat: 57.4667
lon: -130.75
surface_form: Arctic Lake
instance_of: Plateau
countries: Canada
coordinates: lat: 57.3
lon: -130.767
The MEVC is one of the largest volcanic complexes in North America, covering about and comprising about of volcanic material. After Level Mountain, the MEVC is the largest eruptive centre in the Northern Cordilleran Volcanic Province which extends from northwestern British Columbia northwards through Yukon into easternmost Alaska.

Geographic entities mentioned:
surface_form: Northern Cordilleran Volcanic Province
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7156
lon: -130.634
They reached a maximum thickness of more than near their source to only a few metres thick at their terminus. Disruption of the local drainage system by lava flows originating from a cluster of small satellitic cones southeast of the Raspberry shield volcano resulted in the formation of so-named Raspberry Lake in the upper Little Iskut River valley.

Geographic entities mentioned:
surface_form: Little Iskut River
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.448889
lon: -130.268611
These flows range in thickness from about near the centre of Artifact Ridge to around the perimeter, suggesting their source was located near Artifact Ridge. This is supported by the existence of dikes along the northern side of Artifact Creek valley which may have been feeders for the overlying trachybasalt flows.

Geographic entities mentioned:
surface_form: Artifact Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.41635
lon: -130.53728
Armadillo eruptive period. The next eruptive period, the Armadillo period, occurred between 7 and 6 million years ago. It began with explosive activity from a vent at Cartoona Ridge which produced long ash flows and an air-fall pumice deposit that covers an area of several hundred square kilometres.

Geographic entities mentioned:
surface_form: Cartoona Ridge
instance_of: Mountain
coordinates: lat: 57.60666666666667
lon: -130.6147222222222
Eventually bulbous mounds of trachyte and rhyolite covered much of the southeastern highlands of the MEVC; these domes were subsequently eroded to form clastic deposits. Rapid evacuation of a shallow magma chamber nearly south of Cartoona Ridge resulted in the formation of the wide Armadillo Peak caldera.

Geographic entities mentioned:
surface_form: Armadillo Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5383
lon: -130.56
Other volcanic centres were active during the Armadillo eruptive period. Tadeda Peak and the IGC Centre, both satellitic vents of the Armadillo Peak caldera, produced trachyte and rhyolite. Alkali basalt, hawaiite and trachybasalt flows erupted from Sezill Volcano and the Little Iskut shield volcano, many of which are exposed along the Mess Creek Escarpment.

Geographic entities mentioned:
surface_form: Tadeda Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5422
lon: -130.616
Alkali basalt, hawaiite and trachybasalt flows erupted from Sezill Volcano and the Little Iskut shield volcano, many of which are exposed along the Mess Creek Escarpment. The thickest sections of Armadillo basalt flows are exposed in Sezill Creek canyon, Kadeya Creek canyon and near the southwestern end of Raspberry Pass where they reach thicknesses of up to.

Geographic entities mentioned:
surface_form: Sezill Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.69967
lon: -130.88724
surface_form: Kadeya Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.79967
lon: -130.87063
Lava flows from Gamma Peak buried gently sloping alluvial fans on the northern and western flanks of the Armadillo Highlands. An eroded remnant of this volcano forms a prominent rock pinnacle just southeast of Coffee Crater called Cartoona Peak; Kaia Bluff north of Cartoona Peak is also a remnant of Gamma Peak.

Geographic entities mentioned:
surface_form: Coffee Crater
instance_of: Mountain
countries: Canada
coordinates: lat: 57.63
lon: -130.67
surface_form: Cartoona Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.6067
lon: -130.615
Lost Peak consists of volcanic ejecta that was deposited in both subaerial and subaqueous environments; the subaqueous material was deposited in a lake that may have formed between the erupting volcano and a lobe of glacial ice. Exile Hill formed on the southwesternmost edge of the MEVC, most of which was engulfed by younger lava that had flowed to the north and west.

Geographic entities mentioned:
surface_form: Exile Hill
instance_of: Mountain
countries: Canada
coordinates: lat: 57.3783
lon: -130.825
Formation of the Spectrum Dome was followed by evacuation of the magma chamber, resulting in the creation of a wide caldera which was eventually buried by lava from subsequent eruptions. Yeda Peak, a high pinnacle in the middle of the Spectrum Range, was the site of an explosive eruption late in Spectrum time that resulted in the formation of a crater.

Geographic entities mentioned:
surface_form: Yeda Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.3811
lon: -130.678
Erosional remnants of Kitsu Member alkali basalt flows cap the higher summits of the Spectrum Range where they overlie the unmodified upper surface of the original dome. The original dome was higher in elevation as evidenced by the thick, gently dipping trachyte flows forming the summit of Kitsu Peak, the highest point of the Spectrum Range. Pyramid eruptive period.

Geographic entities mentioned:
surface_form: Kitsu Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.4246
lon: -130.6906
The second eruptive period resulted in the creation of the Pillow Ridge Formation which consists mainly of alkali basalt. This geological formation is confined to Pillow Ridge and Tsekone Ridge at the northern end of the MEVC. The third eruptive period produced the Edziza Formation which consists mainly of trachyte that overlies the Ice Peak Formation. Ice Peak eruptive period.

Geographic entities mentioned:
surface_form: Pillow Ridge
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7594
lon: -130.652
surface_form: Tsekone Ridge
instance_of: Mountain
countries: Canada
coordinates: lat: 57.77
lon: -130.69
Volcanism initially began on the southern flank of Sphinx Dome where pyroclastic material mixed with meltwater from residual ice to produce highly mobile debris flows and lahars. Lava flows advanced across the glaciated surface as successive eruptions built Ice Peak, resulting in the formation of narrow meltwater lakes that were displaced as the lava flows continued to advance down slope.

Geographic entities mentioned:
surface_form: Ice Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.6906
lon: -130.635
Two thick lobes of trachyte lava issued from satellitic domes on the western flank of Ice Peak during this eruptive period, both of which were deposited onto the Big Raven Plateau. The southern lobe, Koosick Bluff, ranges in elevation from and is bounded by cliffs that rise to a nearly flat surface.

Geographic entities mentioned:
surface_form: Koosick Bluff
instance_of: Mountain
countries: Canada
coordinates: lat: 57.6739
lon: -130.725
With a length of nearly and a width of more than, Koosick Bluff is the largest of the two lava lobes. The northern and smaller lobe, Ornostay Bluff, is similar in composition and structure to Koosick Bluff; it has a potassium–argon date of 1.5 ± 0.4 million years which may be due to excess argon.

Geographic entities mentioned:
surface_form: Ornostay Bluff
instance_of: Mountain
countries: Canada
coordinates: lat: 57.699722222222
lon: -130.70388888889
Subsequent basalt flows travelled to the southeast and northwest, the southeasterly flows entering the lava-dammed lake to create pillow lava. A circular volcanic plug called The Neck formed southeast of Ice Peak on the northern side of Sorcery Ridge during this eruptive period.

Geographic entities mentioned:
surface_form: Sorcery Ridge
instance_of: Mountain
coordinates: lat: 57.65606944444444
lon: -130.61504166666666
Volcanism on the southeastern rim of the summit crater created Nanook Dome; lava from this dome flowed down the exterior flanks of the stratovolcano and also into the summit crater to form lava lakes. Triangle Dome and Glacier Dome formed on the western and northeastern flanks of Mount Edziza, respectively; Triangle Dome may be the product of subglacial volcanism.

Geographic entities mentioned:
surface_form: Glacier Dome
instance_of: Mountain
countries: Canada
coordinates: lat: 56.4029
lon: -130.9166
Arctic Lake eruptive period. The Arctic Lake eruptive period 0.71 million years ago created at least seven basaltic volcanoes on and adjacent to the Arctic Lake Plateau. Lava fountaining at the extreme northern end of the Arctic Lake Plateau created the Outcast Hill cinder cone which blocked westerly flowing streams to create a temporary lake against its eastern side.

Geographic entities mentioned:
surface_form: Outcast Hill
instance_of: Mountain
countries: Canada
coordinates: lat: 57.39
lon: -130.774
Lava from Outcast Hill flowed into the lake, but most of it travelled to the northwest towards the Mess Creek Escarpment. Tadekho Hill, a cinder cone to the south, formed on top of a high remnant of Spectrum trachyte. Outcast Hill and Tadekho Hill both formed when the Arctic Lake Plateau was relatively free of glacial ice.

Geographic entities mentioned:
surface_form: Tadekho Hill
instance_of: Mountain
countries: Canada
coordinates: lat: 57.3503
lon: -130.785
The Arctic Lake Plateau was subsequently covered with ice as glaciers advanced from the neighbouring Spectrum Range. Subglacial volcanism at the height of this glacial advance created Wetalth Ridge, a subglacial mound near the middle of the plateau. This was followed by the eruption of four other volcanoes on the Arctic Lake Plateau during the waning stages of glaciation.

Geographic entities mentioned:
surface_form: Wetalth Ridge
instance_of: Mountain
countries: Canada
coordinates: lat: 57.2275
lon: -130.786
Lava from Klastline Cone entered Kakiddi Valley where it blocked Kakiddi Creek and then flowed north across dry gravel bars to the confluence with Klastline Valley, temporarily damming the Klastline River to form a large shallow lake. Most of the lava continued to flow westward through Klastline Valley and reached the Stikine River.

Geographic entities mentioned:
surface_form: Kakiddi Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.872778
lon: -130.425556
MEVC volcanic deposits of Late Pleistocene and Early Holocene age are largely basaltic in composition, but their exact ages and chemical compositions are not well-known. Therefore, the MEVC has been suggested as a potential source for these two tephra layers along with Hoodoo Mountain, Heart Peaks and Level Mountain. Snowshoe Lava Field.

Geographic entities mentioned:
surface_form: Hoodoo Mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 56.772222222222
lon: -131.29444444444
surface_form: Heart Peaks
instance_of: Mountain
countries: Canada
coordinates: lat: 58.5989
lon: -131.963
Snowshoe Lava Field. One of the first volcanoes to erupt during the Big Raven eruptive period was Tennena Cone which formed high on the western flank of Ice Peak. It issued basaltic magma under an ice sheet during the Last Glacial Maximum, under an expansion of Mount Edziza's ice cap during the Younger Dryas between 12,900 and 11,600 years ago or during a more recent glacial advance.

Geographic entities mentioned:
surface_form: Tennena Cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.68416666666667
lon: -130.66222222222223
Two unnamed volcanoes also in the Snowshoe Lava Field formed subglacially south of Tennena Cone. After the ice retreated from lower elevations, renewed volcanism in the Snowshoe Lava Field constructed Cocoa Crater, Coffee Crater, Keda Cone and other subaerial cinder cones by lava fountaining.

Geographic entities mentioned:
surface_form: Cocoa Crater
instance_of: Mountain
countries: Canada
coordinates: lat: 57.65
lon: -130.7
After the ice retreated from lower elevations, renewed volcanism in the Snowshoe Lava Field constructed Cocoa Crater, Coffee Crater, Keda Cone and other subaerial cinder cones by lava fountaining. Their construction was accompanied by the eruption of very large lava flows that travelled west into the valleys of Sezill Creek and Taweh Creek at the southwestern end of the Big Raven Plateau.

Geographic entities mentioned:
surface_form: Taweh Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.71638
lon: -130.97063
A fissure eruption from The Saucer south of Tencho Glacier issued lava flows that travelled west into Taweh Creek and east into Shaman Creek; this was one of the most recent eruptions in the Snowshoe Lava Field. Arctic Lake Plateau and east slope centres. At least three eruptive centres were active on the deeply eroded eastern flank of Mount Edziza during Big Raven time.

Geographic entities mentioned:
surface_form: Shaman Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.61636
lon: -130.40395
Arctic Lake Plateau and east slope centres. At least three eruptive centres were active on the deeply eroded eastern flank of Mount Edziza during Big Raven time. Cinder Cliff in the northern fork of Tenchen Creek valley formed when an eruption of basaltic magma ponded against an ice dam and engulfed debris such as moraine and talus.

Geographic entities mentioned:
surface_form: Tenchen Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.76636
lon: -130.43724
Its terminus lies between Kakiddi and Nuttlude lakes where it is well exposed for. Two Big Raven centres formed at the southern end of the MEVC. The southernmost eruptive centre, Nahta Cone, erupted about southwest of the Spectrum Range near the northern edge of the Arctic Lake Plateau and produced a narrow, long basaltic lava flow that travelled northward into the head of Nahta Creek.

Geographic entities mentioned:
surface_form: Nahta Cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.3083
lon: -130.821
Extending roughly west and north of Nahta Cone are two tephra deposits; their distribution suggests the volcano was in eruption at least twice during two differing wind directions. The other eruptive centre is a now-destroyed cinder cone that formed on the unstable southern flank of Kuno Peak at the southwestern end of the Spectrum Range.

Geographic entities mentioned:
surface_form: Kuno Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.3763
lon: -130.7398
Later volcanism created the three Triplex Cones north of Storm Cone which issued a long series of lava flows extending northwesterly to near the south shore of Buckley Lake. Renewed eruptive activity formed Sidas Cone and Twin Cone apart, both of which are products of simultaneous lava fountaining from more than one vent.

Geographic entities mentioned:
surface_form: Sidas Cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.8589
lon: -130.628
Eve Cone and Williams Cone were created apart by the latest Desolation Lava Field eruptions, which issued lava flows more than long that reached Buckley Lake and the Klastline River, respectively. Willow twigs preserved in ejecta from Williams Cone have yielded a radiocarbon date of 610 CE ± 150 years.

Geographic entities mentioned:
surface_form: Eve Cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.81305555555556
lon: -130.67555555555555
surface_form: Williams Cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.78
lon: -130.599
Lava flows from the two oldest cones travelled to the west and most likely cascaded down the escarpment into Mess Creek valley, but no evidence of this phenomenon has been found on or below the escarpment. The youngest cinder cone, The Ash Pit, formed at the south end of the Mess Lake Lava Field on the northern side of Nagha Creek.

Geographic entities mentioned:
surface_form: The Ash Pit
instance_of: Mountain
countries: Canada
coordinates: lat: 57.45
lon: -130.78
The Ash Pit eruption, which may be the most recent of the MEVC, issued mainly pyroclastic ejecta in the form of ash and cinders; much of this material was blown to the north-northeast by a strong, uniform wind during eruption and deposited onto the Kitsu Plateau. Some lava did, however, flow to the northwest through Nagha Creek valley towards Mess Lake in Mess Creek valley.

Geographic entities mentioned:
surface_form: Mess Lake
instance_of: Lake
countries: Canada
coordinates: lat: 57.4667
lon: -130.883
History. The dolmen dates to the Neolithic, around 3000 BC. It was used for interments in which the cremated remains were placed in the tomb, often accompanied by grave goods, including tools, beads and pottery. The tomb may be aligned so that its portal points towards Slieve Gullion and/or the setting sun at the summer solstice.

Geographic entities mentioned:
surface_form: Slieve Gullion
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.133333333333
lon: -6.4333333333333
Cooking Lake (Alberta). Cooking Lake is a lake in Alberta, Canada. It is located in Strathcona County, east-southeast of Edmonton. Cooking Lake Water Aerodrome is located on this lake. Cooking Lake's name is a calque of its Cree language name.

Geographic entities mentioned:
surface_form: cooking lake
instance_of: Lake
countries: Canada
coordinates: lat: 53.4331
lon: -113.029
It was inaugurated in 2004. Within its extension is part of the former Walls of Lima. The park is located between the Rímac River and the historic centre of Lima. History. During the administration of Luis Castañeda Lossio, a section of the remains of the left bank of the Rímac River was recovered and which now forms the park.

Geographic entities mentioned:
surface_form: Rímac River
instance_of: Watercourse
countries: Peru
coordinates: lat: -12.032222222222
lon: -77.141111111111
The park is located between the Rímac River and the historic centre of Lima. History. During the administration of Luis Castañeda Lossio, a section of the remains of the left bank of the Rímac River was recovered and which now forms the park. In this it is possible to see remains of the bases that the cutwater had, the work of the Franciscans in 1610.

Geographic entities mentioned:
surface_form: Rímac River
instance_of: Watercourse
countries: Peru
coordinates: lat: -12.032222222222
lon: -77.141111111111
They also joined to create and promote an artistic salon which came to be known as the &quot;Exposición Anual de Bellas Artes Venezolanas&quot;. Goering presented over 50 drawings and watercolors at their first exhibition in 1872. Later that same year, he and Spence participated in an expedition to climb the Pico Naiguatá. Goering returned to Germany in 1874. Writings and honors.

Geographic entities mentioned:
surface_form: Pico Naiguatá
instance_of: Mountain
countries: Venezuela
coordinates: lat: 10.54333333
lon: -66.7825
When the lake is at the normal summer level, a boat may be used to access remote trailheads such as Hazel Creek. From the observation tower on Kuwohi, on a clear day the lake can be seen nearly a mile below. While the maximum controlled elevation of the lake (top of dam gates) is, the normal Summer surface elevation is.

Geographic entities mentioned:
surface_form: Kuwohi
instance_of: Mountain
countries: United States
coordinates: lat: 35.562777777778
lon: -83.498611111111
Zgornji Motnik. Zgornji Motnik (;) is a dispersed settlement in the hills north of Motnik in the Tuhinj Valley in the Municipality of Kamnik in the Upper Carniola region of Slovenia. It includes the hamlets of Bela, Koprivše, Srobotno, Vrh, and Brezovica.

Geographic entities mentioned:
surface_form: Tuhinj Valley
instance_of: Valley
countries: Slovenia
coordinates: lat: 46.221413888889
lon: 14.775925
Its business runs a production facility with its own shrimp processing line and hatchery in Chittagong, a deep-sea fishing fleet in the Bay of Bengal, a purpose-built processing plant and head office in Manchester, and a distribution operation in The Netherlands. Operations.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
Provata. Provata () is an area of Mount Athos that belongs to the Monastery of Great Lavra. It is close to the Monastery of Karakallou. This is where many people place the Skete of Glossia, which flourished in the 14th century. Gregory Palamas lived in this skete in the 14th century. At the beginning of the century there were 17 cells inhabited by about 100 monks.

Geographic entities mentioned:
surface_form: Mount Athos
instance_of: Mountain
countries: Greece
coordinates: lat: 40.15833333333333
lon: 24.327222222222222
The Roman army received a warm welcome from the populace, which was favourably impressed by its restraint. While Belisarius himself took possession of the royal palace, seated himself on the king's throne, and consumed the dinner which Gelimer had confidently ordered to be ready for his own victorious return, the fleet entered the Lake of Tunis and the army was billeted throughout the city.

Geographic entities mentioned:
surface_form: Lake of Tunis
instance_of: Lake
countries: Tunisia
coordinates: lat: 36.816666666667
lon: 10.25
She is part of a generation of female painters who followed in the footsteps of the original male Papunya Tula artists. Biography. Yukultji Napangati was born north of Kiwirrkurra near Lake Mackay in the Gibson Desert of Western Australia. Living as a nomad, she spent the early years of her life learning about her country, such as the geography, topography, vegetation, fauna, weather, and seasons.

Geographic entities mentioned:
surface_form: Lake Mackay
instance_of: Lake
countries: Australia
coordinates: lat: -22.5
lon: 128.58333333333
Bahram Vallis. Bahram Vallis is an ancient river valley in the Lunae Palus quadrangle of Mars at 20.7° north latitude and 57.5° west longitude. It is about 302 km long and was named after the word for 'Mars' in Persian. Bahram Vallis is located midway between Vedra Valles and lower Kasei Valles. It is basically a single trunk valley, with scalloped walls in some places.

Geographic entities mentioned:
surface_form: Kasei Valles
instance_of: Valley
coordinates: lat: 25.14
lon: 297.12
surface_form: bahram vallis
instance_of: Valley
coordinates: lat: 20.42
lon: 302.86
Bahram Vallis. Bahram Vallis is an ancient river valley in the Lunae Palus quadrangle of Mars at 20.7° north latitude and 57.5° west longitude. It is about 302 km long and was named after the word for 'Mars' in Persian. Bahram Vallis is located midway between Vedra Valles and lower Kasei Valles. It is basically a single trunk valley, with scalloped walls in some places.

Geographic entities mentioned:
surface_form: bahram vallis
instance_of: Valley
coordinates: lat: 20.42
lon: 302.86
Sleeping Beauty Mountain (Kalinga). Sleeping Beauty Mountain (also known as Mount Patukan, Mount Mating-oy Dinayao, Mount Mantingoy) is a mountain ridge in Kalinga province of the Philippines. The mountain is called as such because the silhouette of the northern ridge resembles a sleeping woman.

Geographic entities mentioned:
surface_form: sleeping beauty mountain
instance_of: Mountain
countries: Philippines
coordinates: lat: 17.262222222222
lon: 121.18333333333
Doubletop Mountain (Maine). Doubletop Mountain is a mountain located in Piscataquis County, Maine, in Baxter State Park. According to Fannie Hardy Eckstorm, the mountain's Indigenous name was Psinskihegan-I-Outop. Psinskihegan means notch and I-Outop means head. in 1828 in the Survey of Maine, Moses Greenleaf called the mountain a variation Chinskihegan or Outop.

Geographic entities mentioned:
surface_form: doubletop mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.9359
lon: -69.0612
surface_form: doubletop mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.0276
lon: -74.5282
HIS ASHES WERE GIVEN TO THE WINDS
AT THIS PLACE AUGUST 20, 1926, AT
Keppele Hall's wife, Fanny Hall, was the first American woman to serve as foreman of a grand jury. Geography. Doubletop Mountain stands within the watershed of Nesowadnehunk Stream, which drains into the West Branch of the Penobscot River, and into Penobscot Bay. It is flanked to the southwest by Squaw's Bosom.

Geographic entities mentioned:
surface_form: doubletop mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.9359
lon: -69.0612
surface_form: doubletop mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.0276
lon: -74.5282
Loch Assynt. Loch Assynt () is a freshwater loch in Sutherland, Scotland, north-east of Lochinver. Situated in a spectacular setting between the heights of Canisp, Quinag, and, it receives the outflow from Lochs Awe, and Loch Leitir Easaidh. It discharges into the sea at Loch Inver, via the river Inver.

Geographic entities mentioned:
surface_form: Canisp
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 58.12125
lon: -5.0521
surface_form: Quinag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 58.215061111111
lon: -5.0505305555556
surface_form: Lochs Awe
instance_of: Lake
countries: United Kingdom
coordinates: lat: 58.083333333333
lon: -4.9666666666667
surface_form: Loch Leitir Easaidh
instance_of: Lake
countries: United Kingdom
coordinates: lat: 58.190023
lon: -5.117455
Loch Assynt. Loch Assynt () is a freshwater loch in Sutherland, Scotland, north-east of Lochinver. Situated in a spectacular setting between the heights of Canisp, Quinag, and, it receives the outflow from Lochs Awe, and Loch Leitir Easaidh. It discharges into the sea at Loch Inver, via the river Inver.

Geographic entities mentioned:
surface_form: loch assynt
instance_of: Lake
countries: United Kingdom
coordinates: lat: 58.176347
lon: -5.053878
Situated in a spectacular setting between the heights of Canisp, Quinag, and, it receives the outflow from Lochs Awe, and Loch Leitir Easaidh. It discharges into the sea at Loch Inver, via the river Inver. The general trend of the loch is west-northwest and east-southeast, while the western end bends sharply at Loch Assynt lodge to the southwest. The loch is long, and about in maximum breadth.

Geographic entities mentioned:
surface_form: loch assynt
instance_of: Lake
countries: United Kingdom
coordinates: lat: 58.176347
lon: -5.053878
The elevation of the loch's surface above sea level varies with the levels of rainfall but has been measured as. The Mermaid of Assynt. Whispered amongst the locals of Inchnadamph, the area surrounding the castle, legend tells of MacLeod's lost daughter, Eimhir, and her continued presence at Loch Assynt.

Geographic entities mentioned:
surface_form: loch assynt
instance_of: Lake
countries: United Kingdom
coordinates: lat: 58.176347
lon: -5.053878
Dardano Fenulli was instead assigned to the &quot;Cavalleggeri di Lucca&quot; Cavalry Regiment, and left for Tripolitania where he participated in the final stages of the war. During the First World War he fought on Cima Bocche and the Colbricon, in the Lagorai mountains; he lost his brother, also named Saverio, killed in action on the Karst Plateau during the Tenth Battle of the Isonzo.

Geographic entities mentioned:
surface_form: Cima Bocche
instance_of: Mountain
countries: Italy
coordinates: lat: 46.3544
lon: 11.7517
Shalkar city lies by the northeastern lakeshore. The lake provides water to the city and adjacent railway stations. Geography. Shalkar is located km to the NNW of the Aral Sea. It lies in the Shalkar Basin, a wide tectonic depression between the Mugalzhar Hills to the west and the Barsuki Desert to the east. The Kauylzhyr river flows from the north into the northern end.

Geographic entities mentioned:
surface_form: Aral Sea
instance_of: Lake
countries: Kazakhstan
Uzbekistan
Russian Empire
Soviet Union
coordinates: lat: 45
lon: 60
Shalkar (lake, Aktobe Region). Shalkar () is a brackish lake in Shalkar District, Aktobe Region, Kazakhstan. Shalkar city lies by the northeastern lakeshore. The lake provides water to the city and adjacent railway stations. Geography. Shalkar is located km to the NNW of the Aral Sea.

Geographic entities mentioned:
surface_form: shalkar (lake, aktobe region)
instance_of: Lake
countries: Kazakhstan
Russian Empire
Soviet Union
coordinates: lat: 47.81388889
lon: 59.59166667
The park has 8 tennis courts, an elaborate soft surface children's playground, a bathhouse and a boat pond. The park is best known for its South American monk parakeet nests. At 51st street, there is an overpass leading from the park to the bike path between Lake Shore Drive and Lake Michigan. Boat Pond.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Makimuku Site. The is an archaeological site with the traces of a late-Yayoi period (2nd century) to early-Kofun period (4th century) settlement located at the northwest foot of Mount Miwa of the city of Sakurai, Nara Prefecture, in the Kansai region of Japan. It was designated a National Historic Site in 2013. Overview.

Geographic entities mentioned:
surface_form: Mount Miwa
instance_of: Mountain
countries: Japan
coordinates: lat: 34.535
lon: 135.86666666667
Location. The peak is located at which is 960 m north-northwest of Needle Peak, 1.08 km south-southeast of Preslav Crag, 3.25 km southwest of Peshev Peak and 1.25 km northeast of Radomir Knoll (Bulgarian mapping in 2005 and 2009).

Geographic entities mentioned:
surface_form: Preslav Crag
instance_of: Mountain
coordinates: lat: -62.710194444444
lon: -60.180138888889
surface_form: needle peak
instance_of: Mountain
coordinates: lat: -62.7333
lon: -60.1833
Ludogorie Peak. Ludogorie Peak (,) is a peak rising to 350 m in Friesland Ridge, Tangra Mountains in eastern Livingston Island, South Shetland Islands in Antarctica. The peak overlooks Prespa Glacier to the west and south, Macy Glacier to the northeast, and Brunow Bay to the east, and is named after Ludogorie region in northeastern Bulgaria. Location.

Geographic entities mentioned:
surface_form: ludogorie peak
instance_of: Mountain
coordinates: lat: -62.719583333333
lon: -60.175
The narrowing of the valley southwestwards is caused by the Stillwater Range, its north section which turns to trend due-northeast. The low elevation Buena Vista Hills, and Chocolate Butte, lie between the Carson Sink and the southwest Buena Vista Valley. This hilly region is located in a sub-valley region, named &quot;Antelope Valley&quot;. Access.

Geographic entities mentioned:
surface_form: antelope valley
instance_of: Valley
countries: United States
coordinates: lat: 39.8858
lon: -117.328
surface_form: antelope valley
instance_of: Valley
countries: United States
coordinates: lat: 38.7367
lon: -119.41
surface_form: antelope valley
instance_of: Valley
countries: United States
coordinates: lat: 40.1652
lon: -114.339
surface_form: antelope valley
instance_of: Valley
countries: United States
coordinates: lat: 38.7241
lon: -113.923
surface_form: antelope valley
instance_of: Valley
countries: United States
coordinates: lat: 39.5
lon: -116.3
Buena Vista Valley. The Buena Vista Valley is an approximately long valley located in central-east Pershing County, Nevada. Unionville, Nevada lies at its northwest, at the foothills of the Humboldt Range. The valley contains the approximately long Buena Vista Lake Bed, a crescent shaped lakebed adjacent the southeast perimeter of the Humboldt Range. Description.

Geographic entities mentioned:
surface_form: buena vista lake
instance_of: Lake
countries: United States
coordinates: lat: 35.1919
lon: -119.295
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
The narrowing in the north is from the perimeter ranges of the Humboldt Range, west and the East Range, east. The valley is at its widest at the north end of the Buena Vista Lake Bed, about 13-mi. The southwest is a region connected to the northwest of the Carson Sink.

Geographic entities mentioned:
surface_form: buena vista lake
instance_of: Lake
countries: United States
coordinates: lat: 35.1919
lon: -119.295
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
Buena Vista Valley. The Buena Vista Valley is an approximately long valley located in central-east Pershing County, Nevada. Unionville, Nevada lies at its northwest, at the foothills of the Humboldt Range. The valley contains the approximately long Buena Vista Lake Bed, a crescent shaped lakebed adjacent the southeast perimeter of the Humboldt Range. Description.

Geographic entities mentioned:
surface_form: buena vista valley
instance_of: Valley
countries: United States
coordinates: lat: 40.3564
lon: -117.983
Buena Vista Valley. The Buena Vista Valley is an approximately long valley located in central-east Pershing County, Nevada. Unionville, Nevada lies at its northwest, at the foothills of the Humboldt Range. The valley contains the approximately long Buena Vista Lake Bed, a crescent shaped lakebed adjacent the southeast perimeter of the Humboldt Range. Description.

Geographic entities mentioned:
surface_form: buena vista valley
instance_of: Valley
countries: United States
coordinates: lat: 40.3564
lon: -117.983
surface_form: long valley
instance_of: Landform
countries: United States
coordinates: lat: 37.716666666667
lon: -118.88416666667
surface_form: long valley
instance_of: Valley
countries: United States
coordinates: lat: 39.6833
lon: -115.722
surface_form: long valley
instance_of: Valley
countries: United States
coordinates: lat: 37.3789
lon: -112.573
Description. The Buena Vista Valley is an approximately north–south trending valley, and crescent shaped narrowing both due-north in its north end, and due-southwest in the south. The narrowing in the north is from the perimeter ranges of the Humboldt Range, west and the East Range, east. The valley is at its widest at the north end of the Buena Vista Lake Bed, about 13-mi.

Geographic entities mentioned:
surface_form: buena vista valley
instance_of: Valley
countries: United States
coordinates: lat: 40.3564
lon: -117.983
The narrowing of the valley southwestwards is caused by the Stillwater Range, its north section which turns to trend due-northeast. The low elevation Buena Vista Hills, and Chocolate Butte, lie between the Carson Sink and the southwest Buena Vista Valley. This hilly region is located in a sub-valley region, named &quot;Antelope Valley&quot;. Access.

Geographic entities mentioned:
surface_form: buena vista valley
instance_of: Valley
countries: United States
coordinates: lat: 40.3564
lon: -117.983
Access. The south of Buena Vista Valley can be accessed from the west via Interstate 80, north of Lovelock, via Coal Canyon Road; the road is paved to the valley's south end. The valley's north has Nevada State Route 400 traversing due-south from Mill City on I-80 to Unionville at the west foothills of the Humboldt Range. Numerous unimproved roads extend through all areas of the valley.

Geographic entities mentioned:
surface_form: buena vista valley
instance_of: Valley
countries: United States
coordinates: lat: 40.3564
lon: -117.983
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
The southwest is a region connected to the northwest of the Carson Sink. The narrowing of the valley southwestwards is caused by the Stillwater Range, its north section which turns to trend due-northeast. The low elevation Buena Vista Hills, and Chocolate Butte, lie between the Carson Sink and the southwest Buena Vista Valley.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
Access. The south of Buena Vista Valley can be accessed from the west via Interstate 80, north of Lovelock, via Coal Canyon Road; the road is paved to the valley's south end. The valley's north has Nevada State Route 400 traversing due-south from Mill City on I-80 to Unionville at the west foothills of the Humboldt Range. Numerous unimproved roads extend through all areas of the valley.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
Sam's Lake. &quot;Sam's Lake&quot; is a horror film written and directed by Andrew C. Erin which premiered in 2006 at the Tribeca Film Festival. The film was based on actual events that took place at Sam's Lake, Ontario. Starring Sandrine Holt, Fay Masterson, and William Gregory Lee, the film was shot at ten locations in Nanaimo, Nanaimo Lakes, Cedar, and Yellow Point, British Columbia. Synopsis.

Geographic entities mentioned:
surface_form: Nanaimo Lakes
instance_of: Group of lakes
countries: Canada
coordinates: lat: 49.09965
lon: -124.18602
Precipitation is low and erratic year-round, and primarily occurs during the summer. 20th century. The station was first known as Mount Conner Station (after Mount Conner) in the 1930s, when it was first taken up by Paddy DeConlay as a sheep station. Abraham Andrews leased Mt Conner Station in 1940, and named it Curtin Springs Station after John Curtin.

Geographic entities mentioned:
surface_form: Mount Conner
instance_of: Mountain
countries: Australia
coordinates: lat: -25.492777777778
lon: 131.89777777778
The station has a collection of birds in multiple aviaries around the homestead. All birds have been rescued after an injury or have been bred from captive animals so they are unable to be released into the wild. Local tours include parts of the Amadeus Salt Lake Chain and Mount Conner, which is located on the private property of Curtin Springs Station.

Geographic entities mentioned:
surface_form: Amadeus Salt Lake Chain
instance_of: Lake
countries: Australia
coordinates: lat: -24.75
lon: 130.91666666667
surface_form: Mount Conner
instance_of: Mountain
countries: Australia
coordinates: lat: -25.492777777778
lon: 131.89777777778
Rugova Canyon. 6b6801my3ilpdcxv5n913u5pavjbd" xml:space="preserve">Rugova Canyon (;, &quot;Rugovska klisura&quot;) or Rugova Gorge () is a river canyon near Peja in western Kosovo. The canyon is located in the Albanian Alps, close to the border with Montenegro. Rugova Canyon offers great opportunities for hikers, rock-climbers and cave explorers.

Geographic entities mentioned:
surface_form: rugovska klisura
instance_of: Valley
countries: Kosovo
coordinates: lat: 42.69222222
lon: 20.16861111
surface_form: rugova canyon
instance_of: Valley
countries: Kosovo
coordinates: lat: 42.69222222
lon: 20.16861111
surface_form: rugova
instance_of: Valley
countries: Kosovo
coordinates: lat: 42.69222222
lon: 20.16861111
Rugova Canyon. 6b6801my3ilpdcxv5n913u5pavjbd" xml:space="preserve">Rugova Canyon (;, &quot;Rugovska klisura&quot;) or Rugova Gorge () is a river canyon near Peja in western Kosovo. The canyon is located in the Albanian Alps, close to the border with Montenegro. Rugova Canyon offers great opportunities for hikers, rock-climbers and cave explorers.

Geographic entities mentioned:
surface_form: rugova canyon
instance_of: Valley
countries: Kosovo
coordinates: lat: 42.69222222
lon: 20.16861111
17th century. In 1601 Alonso de Ribera built Fort Talcahuano to defend remaining Spanish settlements near Concepción and Fort Lonquén on the Lonquén River to secure estancias that provided food to the army. In 1602 Ribera rebuilt the small Fort Colcura and Fort Guanaraque and built a new fort, Santa Fe near the confluence of the Bio Bio and Vergara Rivers.

Geographic entities mentioned:
surface_form: Lonquén River
instance_of: Watercourse
countries: Chile
coordinates: lat: -36.4325
lon: -72.690277777778
After the Polish thaw of 1956, Orbis returned to the international market. It organized foreign visits for Polish tourists, mostly to Eastern Bloc countries. Among the most popular locations, were Bulgarian resorts on the Black Sea coast, Lake Balaton in Hungary, and the Yugoslavian coast on the Adriatic Sea. Furthermore, Orbis offered cruises on the TSS Stefan Batory and rented Soviet ships.

Geographic entities mentioned:
surface_form: Lake Balaton
instance_of: Lake
countries: Hungary
coordinates: lat: 46.85
lon: 17.72
The 1st-century historian, Josephus, who mentions the &quot;eastern gate&quot; in his &quot;Antiquities&quot;, makes note of the fact that this gate was considered within the far northeastern extremity of the inner sacred court. According to the Mishnah, there was formerly a causeway which led out of the Temple Mount eastward over the Kidron Valley, extending as far as the Mount of Olives.

Geographic entities mentioned:
surface_form: Kidron Valley
instance_of: Valley
countries: State of Palestine
coordinates: lat: 31.776972222222224
lon: 35.23897222222222
surface_form: Mount of Olives
instance_of: Mountain
countries: Israel
coordinates: lat: 31.777946
lon: 35.245686
California State Route 139. State Route 139 (SR 139) is a state highway in the U.S. state of California. Running from SR 36 in Susanville north to Oregon Route 39 at the Oregon state line, it forms part of the shortest route between Reno, Nevada, and Klamath Falls, Oregon. SR 139 cuts through much of Modoc National Forest and passes near Antelope Mountain and Tule Lake.

Geographic entities mentioned:
surface_form: Tule Lake
instance_of: Lake
countries: United States
coordinates: lat: 41.909322222222
lon: -121.53304722222
The combined routes continue northerly through another part of the forest and over Adin Pass into the Warm Springs Valley, where SR 139 splits to the northwest near Canby. SR 139 runs northwest and north over mostly flat terrain through the center of the national forest before turning northwest.

Geographic entities mentioned:
surface_form: Warm Springs Valley
instance_of: Valley
countries: United States
coordinates: lat: 33.70055556
lon: -117.3425
SR 139 runs northwest and north over mostly flat terrain through the center of the national forest before turning northwest. The route continues through Newell before cutting across the intermittent Tule Lake as the Lava Beds Highway through the city of Tulelake. During this segment, SR 139 passes directly through the former Tule Lake Segregation Unit, used to house Japanese-Americans during WWII.

Geographic entities mentioned:
surface_form: Tule Lake
instance_of: Lake
countries: United States
coordinates: lat: 41.909322222222
lon: -121.53304722222
A local county road already followed this path, but it was an unpaved road, mostly dirt and gravel but with sections of rock and bad sand. This was close to the present SR 139, with notable deviations around the areas of Hayden Hill, Bieber and Lookout, and Malin, Oregon (as Tule Lake covered SR 139's current location).

Geographic entities mentioned:
surface_form: Tule Lake
instance_of: Lake
countries: United States
coordinates: lat: 41.909322222222
lon: -121.53304722222