Sarmila/GeoWiki-Features huggingface dataset:
Oasis Valley. 80gews4kwckacvl7n26gxpslpvlk5" xml:space="preserve">Oasis Valley is a valley in the Amargosa Desert near Beatty in Nye County, western Nevada. The valley forms part of the southern drainage of Pahute Mesa. The Amargosa River flows through the Oasis Valley between the Bare Mountains and the Bullfrog Hills to the Amargosa Valley. Natural history.

Geographic entities mentioned:
surface_form: Bullfrog Hills
instance_of: Landform
countries: United States
coordinates: lat: 36.958888888889
lon: -116.83277777778
surface_form: Amargosa Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.6333
lon: -116.4
surface_form: oasis valley
instance_of: Valley
countries: United States
coordinates: lat: 36.916666666666664
lon: -116.75916666666667
Natural history. Oasis Valley is a portion of the Upper Amargosa Watershed. It includes geologic features of the Timber Mountain-Oasis Valley caldera complex of the Southwest Nevada volcanic field. The Amargosa toad is endemic to the Oasis Valley section of the Amargosa River, with its threatened population being successfully increased by local citizen efforts.

Geographic entities mentioned:
surface_form: timber mountain
instance_of: Mountain
countries: United States
coordinates: lat: 34.245006
lon: -117.5931091
surface_form: oasis valley
instance_of: Valley
countries: United States
coordinates: lat: 36.916666666666664
lon: -116.75916666666667
Oasis Valley. 80gews4kwckacvl7n26gxpslpvlk5" xml:space="preserve">Oasis Valley is a valley in the Amargosa Desert near Beatty in Nye County, western Nevada. The valley forms part of the southern drainage of Pahute Mesa. The Amargosa River flows through the Oasis Valley between the Bare Mountains and the Bullfrog Hills to the Amargosa Valley. Natural history.

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
Oasis Valley. 80gews4kwckacvl7n26gxpslpvlk5" xml:space="preserve">Oasis Valley is a valley in the Amargosa Desert near Beatty in Nye County, western Nevada. The valley forms part of the southern drainage of Pahute Mesa. The Amargosa River flows through the Oasis Valley between the Bare Mountains and the Bullfrog Hills to the Amargosa Valley. Natural history.

Geographic entities mentioned:
surface_form: oasis valley
instance_of: Valley
countries: United States
coordinates: lat: 36.916666666666664
lon: -116.75916666666667
The valley forms part of the southern drainage of Pahute Mesa. The Amargosa River flows through the Oasis Valley between the Bare Mountains and the Bullfrog Hills to the Amargosa Valley. Natural history. Oasis Valley is a portion of the Upper Amargosa Watershed. It includes geologic features of the Timber Mountain-Oasis Valley caldera complex of the Southwest Nevada volcanic field.

Geographic entities mentioned:
surface_form: oasis valley
instance_of: Valley
countries: United States
coordinates: lat: 36.916666666666664
lon: -116.75916666666667
Natural history. Oasis Valley is a portion of the Upper Amargosa Watershed. It includes geologic features of the Timber Mountain-Oasis Valley caldera complex of the Southwest Nevada volcanic field. The Amargosa toad is endemic to the Oasis Valley section of the Amargosa River, with its threatened population being successfully increased by local citizen efforts.

Geographic entities mentioned:
surface_form: oasis valley
instance_of: Valley
countries: United States
coordinates: lat: 36.916666666666664
lon: -116.75916666666667
Chateauguay Valley Regional High School. Chateauguay Valley Regional (CVR)is a bilingual English/French high school in Ormstown, Quebec, Canada, serving the Chateauguay Valley and Valleyfield area. It is administered by the New Frontiers School Board. Enrolment was approximately 550 as of 2019, but has ranged from 550 to 1500 during the school's history, in accordance with demographic trends.

Geographic entities mentioned:
surface_form: Chateauguay Valley
instance_of: Valley
countries: Canada
coordinates: lat: 45.3611
lon: -73.75
Distribution and habitat. Southern blue gum grows in open forest in mountainous, largely inland country in New South Wales and Victoria. It is found between the Carrai National Park on the Northern Tablelands of New South Wales and the ranges of eastern Victoria.

Geographic entities mentioned:
surface_form: Northern Tablelands
instance_of: Plateau
countries: Australia
coordinates: lat: -30.595277777777778
lon: 151.5
The large Zeya Reservoir is downstream 140 km to the southwest. The park itself stretches 120 km from west to east along the range, and an average of 30 km north to south on the slopes. Although Lake Bolshoye Toko lends its name to the mountains and the park, the lake itself is 30 km to the north of the park on the north slope of the Stanovoy mountains.

Geographic entities mentioned:
surface_form: Lake Bolshoye Toko
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 56.056111111111
lon: 130.88583333333
Ecoregion and climate. The higher elevations of the park are in the Trans-Baikal Bald Mountain tundra ecoregion, making it part of a linked chain of mountain tundra (permafrost, moss and lichen, and bare rock) micro-regions stretching from Lake Baikal (1,300 km to the west of the park) to the Sea of Okhotsk 400 km to the east.

Geographic entities mentioned:
surface_form: Lake Baikal
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.30277778
lon: 108.00472222
Geography. Knockfin is bounded on the west by Curraghnabania and Seltanahunshin townlands and on the east by Corraleehanbeg, Garryfliugh and Prabagh townlands. Its chief geographical features are Sliabh an Iarainn mountain on whose eastern slope it lies, mountain streams, waterfalls, a lime-kiln and dug wells. It is traversed by minor public roads and rural lanes.

Geographic entities mentioned:
surface_form: Sliabh an Iarainn
instance_of: Mountain
countries: Ireland
coordinates: lat: 54.09259722
lon: -7.9721
Mount Shani. Mt. Shani (;;) also known as Shan and Shanloam is a mountain in the Caucasus. It has an elevation of and is on the international border between Georgia and Ingushetia, Russia. The mountain rises approx. nine kilometres to the east of Stepantsminda, Georgia. Access from Georgia is through the Kistinka gorge (alt. Brolistskali), which separates the Khuro massif from Mt. Shani.

Geographic entities mentioned:
surface_form: mount shani
instance_of: Mountain
countries: Georgia
Russia
Russian Empire
Soviet Union
coordinates: lat: 42.675833333333
lon: 44.7575
On a field trip to Mount Hermon in 1906, the agronomist Aaron Aaronsohn discovered Triticum dicoccoides, or emmer wheat, believed to be the &quot;mother of all wheat.&quot; In 1909, he founded an agricultural research station in Atlit where he built up an extensive library and collected geological and botanical samples.

Geographic entities mentioned:
surface_form: Mount Hermon
instance_of: Mountain
countries: Lebanon
Israel
Syria
coordinates: lat: 33.4
lon: 35.85
The station manufactured vaccines against typhus and cholera, and developed methods of pest control to eliminate field mice. The Pasteur Institute affiliated with the station developed a rabies vaccine. Departments for microbiology, biochemistry, bacteriology, and hygiene were opened at the Hebrew University of Jerusalem, founded on Mount Scopus in 1925.

Geographic entities mentioned:
surface_form: Mount Scopus
instance_of: Mountain
countries: Israel
coordinates: lat: 31.7925
lon: 35.244166666667
It has an effective radiated power (ERP) of 20,000 watts. The transmitter is on Sunil Pandit Road in Carson City, amid the towers for other FM and TV stations in the Reno media market. KNCC is a Class A station with an ERP of 54 watts. Its transmitter is atop Elko Mountain. Programming is also heard on numerous FM translators around Nevada and Northern California. Programming.

Geographic entities mentioned:
surface_form: Elko Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.8945
lon: -115.63
It is referred to as the Very High Damage Risk Zone. The regions of Kashmir, the Western and Central Himalayas, North and Middle Bihar, the North-East Indian region, the Rann of Kutch and the Andaman and Nicobar group of islands fall in this zone. Generally, the areas having trap rock or basaltic rock are prone to earthquakes. Zone 4.

Geographic entities mentioned:
surface_form: Kashmir
instance_of: Valley
countries: India
coordinates: lat: 34.0333
lon: 74.6667
Today, the route of railway line from Riverton to Auburn has been converted into a walking/cycle rail trail, known as the Rattler Trail. The Rattler Trail joins the Riesling Trail at Auburn, providing a 43 km route from Riverton, through the heart of the Clare Valley wine region to the North. The Spalding branch line closed in April 1984.

Geographic entities mentioned:
surface_form: Clare Valley
instance_of: Valley
countries: Australia
coordinates: lat: -33.83361111
lon: 138.61
Geographic location. The Molasse basin stretches over 1000 kilometers along the long axis of the Alps, in France, Switzerland, Germany and Austria. The west end is at Lake Geneva, where the basin's outcrop is just 20 km wide. Further to the northeast the basin becomes wider. It forms the subsurface of the Swiss Mittelland and reaches its widest (circa 130 km) in the Bavarian foreland of the Alps.

Geographic entities mentioned:
surface_form: Lake Geneva
instance_of: Lake
countries: Switzerland
France
coordinates: lat: 46.45
lon: 6.55
The west end is at Lake Geneva, where the basin's outcrop is just 20 km wide. Further to the northeast the basin becomes wider. It forms the subsurface of the Swiss Mittelland and reaches its widest (circa 130 km) in the Bavarian foreland of the Alps. From Amstetten to Sankt Pölten the basin forms a narrow band, just 10 km wide. After that it widens again to the east.

Geographic entities mentioned:
surface_form: Mittelland
instance_of: Plateau
countries: Switzerland
coordinates: lat: 47.1167
lon: 7.36667
In the Eastern Alps an external mountain range such as the Jura Mountains never developed. Due to the last phase of tectonic uplift around 5 million years ago, the molasse in the Swiss Plateau, the South Bavarian plain and Eastern Austria is now 350 to 400 meters above sea level at its northern rim, slowly rises southwards and can reach more than 1,000 m at its contact with the Alps. Stratigraphy.

Geographic entities mentioned:
surface_form: Swiss Plateau
instance_of: Plateau
countries: Switzerland
coordinates: lat: 47.1167
lon: 7.36667
Rivière à l'Ours Ouest. The Rivière à l'Ours Ouest () is a tributary of the rivière à l'Ours, flowing through the municipality of Havre-Saint-Pierre, in the Minganie Regional County Municipality, in the administrative region of Côte-Nord, in the province of Quebec, in Canada. Except for the route 138 serving the lower part of the Bear River, this valley is served by winter snowmobile routes.

Geographic entities mentioned:
surface_form: rivière à l'ours
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.24194
lon: -77.9625
surface_form: rivière à l'ours
instance_of: Watercourse
countries: Canada
coordinates: lat: 50.29833305555555
lon: -63.058055
surface_form: rivière à l'ours ouest
instance_of: Watercourse
countries: Canada
coordinates: lat: 50.33345
lon: -63.09859
surface_form: rivière à l'ours
instance_of: Watercourse
countries: Canada
coordinates: lat: 48.646666666667
lon: -72.390555555556
Rivière à l'Ours Ouest. The Rivière à l'Ours Ouest () is a tributary of the rivière à l'Ours, flowing through the municipality of Havre-Saint-Pierre, in the Minganie Regional County Municipality, in the administrative region of Côte-Nord, in the province of Quebec, in Canada. Except for the route 138 serving the lower part of the Bear River, this valley is served by winter snowmobile routes.

Geographic entities mentioned:
surface_form: rivière à l'ours
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.24194
lon: -77.9625
surface_form: rivière à l'ours
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.24194
lon: -77.9625
surface_form: rivière à l'ours
instance_of: Watercourse
countries: Canada
coordinates: lat: 50.29833305555555
lon: -63.058055
surface_form: rivière à l'ours
instance_of: Watercourse
countries: Canada
coordinates: lat: 50.29833305555555
lon: -63.058055
surface_form: rivière à l'ours ouest
instance_of: Watercourse
countries: Canada
coordinates: lat: 50.33345
lon: -63.09859
surface_form: rivière à l'ours
instance_of: Watercourse
countries: Canada
coordinates: lat: 48.646666666667
lon: -72.390555555556
surface_form: rivière à l'ours
instance_of: Watercourse
countries: Canada
coordinates: lat: 48.646666666667
lon: -72.390555555556
Toponymy. The toponym &quot;Rivière à l'Ours Ouest&quot; was formalized on December 5, 1968, at the Place Names Bank of the Commission de toponymie du Québec.

Geographic entities mentioned:
surface_form: rivière à l'ours
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.24194
lon: -77.9625
surface_form: rivière à l'ours
instance_of: Watercourse
countries: Canada
coordinates: lat: 50.29833305555555
lon: -63.058055
surface_form: rivière à l'ours ouest
instance_of: Watercourse
countries: Canada
coordinates: lat: 50.33345
lon: -63.09859
surface_form: rivière à l'ours
instance_of: Watercourse
countries: Canada
coordinates: lat: 48.646666666667
lon: -72.390555555556
Geography. From the mouth of the West Bear River, the current follows the course of the Bear River on towards the south-east, then crosses on east of Victor Bay until bypassing Victor Island, which is part of the north shore of the Estuary of Saint Lawrence. Toponymy.

Geographic entities mentioned:
surface_form: island
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
surface_form: bear river
instance_of: Watercourse
countries: Canada
coordinates: lat: 56.2833
lon: -126.967
surface_form: bear river
instance_of: Watercourse
countries: Canada
coordinates: lat: 56.2833
lon: -126.967
Rivière à l'Ours Ouest. The Rivière à l'Ours Ouest () is a tributary of the rivière à l'Ours, flowing through the municipality of Havre-Saint-Pierre, in the Minganie Regional County Municipality, in the administrative region of Côte-Nord, in the province of Quebec, in Canada. Except for the route 138 serving the lower part of the Bear River, this valley is served by winter snowmobile routes.

Geographic entities mentioned:
surface_form: bear river
instance_of: Watercourse
countries: Canada
coordinates: lat: 56.2833
lon: -126.967
Except for the route 138 serving the lower part of the Bear River, this valley is served by winter snowmobile routes. The surface of the West Bear River is usually frozen from the beginning of November to the end of April, except the rapids areas; however, traffic on the ice is generally safe from late November to early April. Geography.

Geographic entities mentioned:
surface_form: bear river
instance_of: Watercourse
countries: Canada
coordinates: lat: 56.2833
lon: -126.967
Pointe d'Otemma. The Pointe d'Otemma is a mountain of the Swiss Pennine Alps, located south of the lake of Mauvoisin in the canton of Valais. It lies at western end of the chain separating the Brenay Glacier from the Otemma Glacier. On the west side of the mountain lies the Chanrion Hut. The closest locality in the valley is Fionnay.

Geographic entities mentioned:
surface_form: pointe d'otemma
instance_of: Mountain
countries: Switzerland
coordinates: lat: 45.9435
lon: 7.3977777777778
In many Ojibwe communities throughout Canada and the U.S. since the late 20th century, more members have been using the generalized name &quot;Anishinaabe(-g)&quot;. Because many Ojibwe were formerly located around the outlet of Lake Superior, which the French colonists called Sault Ste. Marie for its rapids, the early Canadian settlers referred to the Ojibwe as &quot;Saulteurs&quot;.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
After receiving assurance from their &quot;Allied Brothers&quot; (i.e., Mi'kmaq) and &quot;Father&quot; (i.e., Abenaki) of their safety to move inland, the Anishinaabeg gradually migrated west along the Saint Lawrence River to the Ottawa River to Lake Nipissing, and then to the Great Lakes.

Geographic entities mentioned:
surface_form: Lake Nipissing
instance_of: Lake
countries: Canada
coordinates: lat: 46.283333333333
lon: -80
The latter allied with the Sauk for protection. By the end of the 18th century, the Ojibwe controlled nearly all of present-day Michigan, northern Wisconsin, and Minnesota, including most of the Red River area. They also controlled the entire northern shores of lakes Huron and Superior on the Canadian side and extending westward to the Turtle Mountains of North Dakota.

Geographic entities mentioned:
surface_form: Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
In the United States, many Ojibwe communities safe-guard their burial mounds through the enforcement of the 1990 Native American Graves Protection and Repatriation Act. Several Ojibwe bands in the United States cooperate in the Great Lakes Indian Fish & Wildlife Commission, which manages the treaty hunting and fishing rights in the Lake Superior-Lake Michigan areas.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
In Michigan, the Chippewa-Ottawa Resource Authority manages the hunting, fishing and gathering rights about Sault Ste. Marie, and the resources of the waters of lakes Michigan and Huron. In Canada, the Grand Council of Treaty No. 3 manages the Treaty 3 hunting and fishing rights related to the area around Lake of the Woods. Cuisine.

Geographic entities mentioned:
surface_form: Lake of the Woods
instance_of: Lake
countries: Canada
United States
coordinates: lat: 49.09027777777778
lon: -95.2388888888889
Nubble Peak. Nubble Peak, also known as The Peak Above The Nubble, is a mountain located in Grafton County, New Hampshire. The mountain is part of the Twin Range of the White Mountains. A rock outcrop on its northwestern ridge is known as The Nubble, but topographic maps identify the formation as Haystack Mountain. Nubble Peak is flanked to the south by North Twin Mountain.

Geographic entities mentioned:
surface_form: haystack mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.00481583
lon: -73.208447
surface_form: haystack mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.6301
lon: -78.8206
surface_form: haystack mountain
instance_of: Mountain
countries: United States
coordinates: lat: 35.355311111111114
lon: -107.94756111111111
surface_form: haystack mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.914
lon: -72.9195
surface_form: haystack mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.17941667
lon: -75.89200556
surface_form: haystack mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.731666666667
lon: -109.16611111111
Nubble Peak. Nubble Peak, also known as The Peak Above The Nubble, is a mountain located in Grafton County, New Hampshire. The mountain is part of the Twin Range of the White Mountains. A rock outcrop on its northwestern ridge is known as The Nubble, but topographic maps identify the formation as Haystack Mountain. Nubble Peak is flanked to the south by North Twin Mountain.

Geographic entities mentioned:
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: nubble peak
instance_of: Mountain
countries: United States
coordinates: lat: 44.222888888889
lon: -71.561533333333
The mountain is officially trailless and is one of New England's hundred highest summits. Nubble Peak stands within the watershed of the Ammonoosuc River, which drains into the upper Connecticut River, and into Long Island Sound in Connecticut. The east and southeast faces of Nubble Peak drain into the Little River, thence into the Ammonoosuc River.

Geographic entities mentioned:
surface_form: long island
instance_of: Landform
countries: United States
coordinates: lat: 46.7269
lon: -90.785
surface_form: nubble peak
instance_of: Mountain
countries: United States
coordinates: lat: 44.222888888889
lon: -71.561533333333
The mountain is part of the Twin Range of the White Mountains. A rock outcrop on its northwestern ridge is known as The Nubble, but topographic maps identify the formation as Haystack Mountain. Nubble Peak is flanked to the south by North Twin Mountain. The mountain is officially trailless and is one of New England's hundred highest summits.

Geographic entities mentioned:
surface_form: north twin mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.2023
lon: -71.5583
surface_form: nubble peak
instance_of: Mountain
countries: United States
coordinates: lat: 44.222888888889
lon: -71.561533333333
surface_form: twin mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.1257
lon: -74.1293
Nubble Peak. Nubble Peak, also known as The Peak Above The Nubble, is a mountain located in Grafton County, New Hampshire. The mountain is part of the Twin Range of the White Mountains. A rock outcrop on its northwestern ridge is known as The Nubble, but topographic maps identify the formation as Haystack Mountain. Nubble Peak is flanked to the south by North Twin Mountain.

Geographic entities mentioned:
surface_form: nubble peak
instance_of: Mountain
countries: United States
coordinates: lat: 44.222888888889
lon: -71.561533333333
Nubble Peak stands within the watershed of the Ammonoosuc River, which drains into the upper Connecticut River, and into Long Island Sound in Connecticut. The east and southeast faces of Nubble Peak drain into the Little River, thence into the Ammonoosuc River. The northwest side of Nubble Peak drains into Haystack Brook, thence into the Ammonoosuc.

Geographic entities mentioned:
surface_form: nubble peak
instance_of: Mountain
countries: United States
coordinates: lat: 44.222888888889
lon: -71.561533333333
The east and southeast faces of Nubble Peak drain into the Little River, thence into the Ammonoosuc River. The northwest side of Nubble Peak drains into Haystack Brook, thence into the Ammonoosuc. The southwest end of Nubble Peak drains to the North Branch of the Gale River, another tributary of the Ammonoosuc River.

Geographic entities mentioned:
surface_form: nubble peak
instance_of: Mountain
countries: United States
coordinates: lat: 44.222888888889
lon: -71.561533333333
Dome Rock. Dome Rock is an andesite formation of the Old Cascades in the Willamette National Forest. The mountain is best known for its hiking trail that goes to the summit. Dome Rock lies in Linn County, Oregon. About 3 miles southeast of Dome Rock is the small town of Detroit.

Geographic entities mentioned:
surface_form: dome rock
instance_of: Mountain
countries: United States
coordinates: lat: 44.7525
lon: -122.20861111111
Milton Lilbourne. Milton Lilbourne is a village and civil parish in the county of Wiltshire, England, in the Vale of Pewsey between Pewsey and Burbage. It is largely a mixed residential area centred on the Manor. The nearest town is Marlborough, to the north.

Geographic entities mentioned:
surface_form: Vale of Pewsey
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.352
lon: -1.851
It is largely a mixed residential area centred on the Manor. The nearest town is Marlborough, to the north. The parish is unusual in that it has a long thin shape and is one of the few to have boundaries on the uplands to both south and north of the Vale. The southern boundary passes by a long barrow and the northern one abuts the prehistoric fort on Martinsell Hill. History.

Geographic entities mentioned:
surface_form: Martinsell Hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 51.37342
lon: -1.74457
Britton Creek. Britton Creek is a tributary of the Tulameen River in British Columbia. This creek is southwest of the old town of Tulameen. Britton Creek is located in a region of British Columbia called the Similkameen. The creek can be reached by road. Britton Creek was originally known as Eagle Creek. It was discovered in 1885 when gold was recovered from the creek.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: britton creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 49.5317
lon: -120.094
Britton Creek. Britton Creek is a tributary of the Tulameen River in British Columbia. This creek is southwest of the old town of Tulameen. Britton Creek is located in a region of British Columbia called the Similkameen. The creek can be reached by road. Britton Creek was originally known as Eagle Creek. It was discovered in 1885 when gold was recovered from the creek.

Geographic entities mentioned:
surface_form: britton creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 49.5317
lon: -120.094
This creek is southwest of the old town of Tulameen. Britton Creek is located in a region of British Columbia called the Similkameen. The creek can be reached by road. Britton Creek was originally known as Eagle Creek. It was discovered in 1885 when gold was recovered from the creek. The gold was mainly close to the mouth of the creek. The creek also yielded placer platinum.

Geographic entities mentioned:
surface_form: britton creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 49.5317
lon: -120.094
surface_form: eagle creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 52.3501
lon: -107.40127
Teahitiʻa. Teahitiʻa (&quot;Standing Fire&quot;) is a submarine volcano, located northeast of the southeast tip of Tahiti of the Society Islands in the Pacific Ocean, with its peak 1450 meters below the water surface. It belongs to the Society hotspot. Teahitiʻa's last eruption occurred in 1985. The seamount has four prominent cones.

Geographic entities mentioned:
surface_form: teahitiʻa
instance_of: Mountain
countries: France
coordinates: lat: -17.57
lon: -148.85
Earthquake swarms in March 1982, July 1983, December 1983, and January 1985 have been associated with submarine eruptions. On 16 March 2008 Teahitiʻa was the epicentre of an earthquake measuring 3.2 on the Richter scale. The weak tremor was felt in Tahiti, causing the beginnings of panic in the population unaccustomed to these seismic phenomena and fearing a tidal wave.

Geographic entities mentioned:
surface_form: teahitiʻa
instance_of: Mountain
countries: France
coordinates: lat: -17.57
lon: -148.85
The park adjoins the Allinagaram Reserved Forest within the proposed Palani Hills Wildlife Sanctuary and National Park.It is a part of Palani hills stretched up to Vandaravu peak. The Westerns Ghats, Anamalai Sub-Cluster, including these parks, is under consideration by the UNESCO World Heritage Committee for selection as a World Heritage Site. Etymology.

Geographic entities mentioned:
surface_form: Vandaravu
instance_of: Mountain
countries: India
coordinates: lat: 10.149
lon: 77.273
The population was 3,121 at the 2020 census. The CDP is considered to be part of the Holland urban area. It is located on the north shore of Lake Macatawa mostly within Holland Charter Township, although a small portion lies within Park Township. Geography. According to the United States Census Bureau, the community has a total area of, of which is land and (32.22%) is water. Demographics.

Geographic entities mentioned:
surface_form: Lake Macatawa
instance_of: Lake
countries: United States
coordinates: lat: 42.778955555555555
lon: -86.16151388888889
ISRO downlinked launch telemetry during the ballistic coasting phase until the radio black-out to avoid data loss in the event of a failure. At an altitude of around, the module's apex cover separated and the parachutes were deployed. CARE splashed down in the Bay of Bengal near the Andaman and Nicobar Islands and was recovered successfully. Chandrayaan.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
Singuttara Hill. Siṅguttara Hill (; also spelt &quot;Theingottara Hill&quot;) is a small hill in Yangon, Myanmar (formerly Burma), crowned by the Shwedagon Pagoda, the most famous pagoda in the country. Tapussa and Bhallika.

Geographic entities mentioned:
surface_form: singuttara hill
instance_of: Mountain
countries: Myanmar
coordinates: lat: 16.79833333
lon: 96.14944444
The two brothers are recorded as the first lay disciples of the Buddha. The Buddha told them the relics should be enshrined in their own land on Singuttara hill, where relics of three previous Buddhas already rested.

Geographic entities mentioned:
surface_form: singuttara hill
instance_of: Mountain
countries: Myanmar
coordinates: lat: 16.79833333
lon: 96.14944444
As of January 28, 2019, XEWT revamped its hours of local news. The station now airs a 90-minute morning newscast at 6:30 a.m. (followed by Que Buen Dia), a full-hour newscast at 2 p.m., a new 90-minute evening newscast at 5 p.m., and a late night newscast at 10:30 p.m. which focuses on all of Baja California, as well as San Diego and the Imperial Valley. Subchannel.

Geographic entities mentioned:
surface_form: Imperial Valley
instance_of: Valley
countries: United States
coordinates: lat: 33.1
lon: -115.5
Gajisan (South Jeolla). Gajisan () is a mountain in South Jeolla Province, southwestern South Korea. It has an elevation of 510 metres.

Geographic entities mentioned:
surface_form: gajisan
instance_of: Mountain
countries: South Korea
coordinates: lat: 35.62111111
lon: 129.00305556
surface_form: gajisan (south jeolla)
instance_of: Mountain
countries: South Korea
coordinates: lat: 34.82
lon: 126.9027
Gajisan (South Jeolla). Gajisan () is a mountain in South Jeolla Province, southwestern South Korea. It has an elevation of 510 metres.

Geographic entities mentioned:
surface_form: gajisan
instance_of: Mountain
countries: South Korea
coordinates: lat: 35.62111111
lon: 129.00305556
surface_form: gajisan
instance_of: Mountain
countries: South Korea
coordinates: lat: 34.82
lon: 126.9027
Spring Creek is a tributary of the Flint River in southwest Georgia in the United States. Rising in the northeastern corner of Clay County, north of Bluffton, the creek flows south to join the Flint River in Lake Seminole, approximately upstream of that river's confluence with the Chattahoochee River to form the Apalachicola River, which flows through Florida to the Gulf of Mexico.

Geographic entities mentioned:
surface_form: Chattahoochee River
instance_of: Watercourse
countries: United States
coordinates: lat: 30.7088028
lon: -84.8638097
It is home to two castles, the &quot;Rocca&quot; (or &quot;Castello Superiore&quot;, known from 1047, and enlarged in the 15th century after its sack by Facino Cane's troops) and the &quot;Castello Inferiore&quot; (15th century). Lake Arignano is located in the comune.

Geographic entities mentioned:
surface_form: Lake Arignano
instance_of: Lake
countries: Italy
coordinates: lat: 45.046
lon: 7.889
Al-Hebbariyah. Al-Hebbariyah, Hebbariyeh, Hebbariya or Hebariya () is a municipality situated in the Hasbaya District of the Nabatieh Governorate in Lebanon. It is located on the southwestern slopes of Mount Hermon near the Lebanon–Syria border, northeast of Rachaya Al Foukhar and is positioned amongst orchards of apricot trees. There it is a roman temple. The village sits c.

Geographic entities mentioned:
surface_form: Mount Hermon
instance_of: Mountain
countries: Lebanon
Israel
Syria
coordinates: lat: 33.4
lon: 35.85
The village sits c. above sea level and the small population is predominantly support the Lebanese Communist party
Roman temple. There is a Roman temple near to the village, opposite the Wadi Shib'a which is the most southern of the Temples of Mount Hermon, a group defined by George Taylor as being south of the main road to Damascus on the west of Mount Hermon, including the Wadi al-Taym area.

Geographic entities mentioned:
surface_form: Mount Hermon
instance_of: Mountain
countries: Lebanon
Israel
Syria
coordinates: lat: 33.4
lon: 35.85
surface_form: Wadi al-Taym
instance_of: Valley
countries: Lebanon
coordinates: lat: 33.4333
lon: 35.7
It has been classified as an Antae temple with an eastern portal that faces Mount Hermon, aligned &quot;as if to catch the first beams of the morning sun rising over Hermon.&quot; The temple has a large basement chamber underneath the cella floors that is thought to have been used for burial. The room is only accessible from the outside of the building.

Geographic entities mentioned:
surface_form: Mount Hermon
instance_of: Mountain
countries: Lebanon
Israel
Syria
coordinates: lat: 33.4
lon: 35.85
Ljosanbotn Station. Ljosanbotn Station () is a railway station on the Bergensbanen railway line located at Ljosanbotn in the Raundalen valley in the municipality of Voss in Vestland county, Norway. The station is served by the Bergen Commuter Rail, operated by Vy Tog, with up to five daily departures in each direction. The station was opened in 1948.

Geographic entities mentioned:
surface_form: Raundalen
instance_of: Valley
countries: Norway
coordinates: lat: 60.6789
lon: 6.56167
All other trails in the area were constructed and are maintained by the Mazamas, a mountaineering organization based out of Portland, Oregon. The Mazamas trails are classified as primitive, are steep and sometimes difficult to follow. The top of Observation Peak offers panoramic views of Mount Hood, Mount Adams, Mount Rainier, Mount Jefferson and the Goat Rocks.

Geographic entities mentioned:
surface_form: Mount Hood
instance_of: Mountain
countries: United States
coordinates: lat: 45.37361111111111
lon: -121.69583333333334
surface_form: Mount Rainier
instance_of: Mountain
countries: United States
coordinates: lat: 46.85166666666667
lon: -121.76027777777777
The creek formed an important part of the Pūkaki portage, connecting the Manukau Harbour and Tāmaki River via Papatoetoe, and was often used by Tāmaki Māori to avoid the Te Tō Waka and Karetu portages, controlled by the people who lived at Mount Richmond.

Geographic entities mentioned:
surface_form: Mount Richmond
instance_of: Mountain
countries: New Zealand
coordinates: lat: -36.9326
lon: 174.839
From 1277–1303, the region was plagued with intense conflict and competition between the Pagan kingdom and Yuan dynasty. The Mongol-Yuan wanted to secure access to the Bay of Bengal, and waged two bloody wars in the region, the First Mongol invasion of Burma which toppled the Pagan kingdom, and the Second Mongol invasion of Burma which drove the Mongols out.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
After conferring with police, the family declined the offers, but they later accepted, and the reward eventually stood at over 950,000 NOK (US $160,000). Volunteers, along with police units, canvassed the neighbourhood and local parks, while search-and-rescue divers from the fire department searched Lake Østensjø, which is near the site of her disappearance.

Geographic entities mentioned:
surface_form: Lake Østensjø
instance_of: Lake
countries: Norway
coordinates: lat: 59.888333333333
lon: 10.826944444444
Temple of Mercury (Puy de Dôme). The Temple of Mercury at Puy de Dôme is a Gallo-Roman trachyte temple built in the 2nd century at the summit of the lava dome. It replaced a 1st-century arkose temple on the same site, which was apparently too small to accommodate the many pilgrims who visited. Its remains were revealed by excavation campaigns in 1875 and at the turn of the century.

Geographic entities mentioned:
surface_form: Puy de Dôme
instance_of: Mountain
countries: France
coordinates: lat: 45.772
lon: 2.9624
We wanted to do this so that visitors understand better, but whether we go above or below, we no longer see the processional system; the result: people will certainly not understand more. Chronology. A first temple was built around 50 CE on the summit of Puy de Dôme. Although objects dating from prior to the Roman conquest have been discovered, no trace of a pre-Roman building has been found.

Geographic entities mentioned:
surface_form: Puy de Dôme
instance_of: Mountain
countries: France
coordinates: lat: 45.772
lon: 2.9624
Mandalay Gazette. The &quot;Myanmar Gazette&quot; (; &quot;Yadanabon Naypyidaw Thadinza&quot;) is a San Gabriel Valley-based Burmese language newspaper intended for overseas Burmese, with a primary focus on Burmese related news in the United States and Canada.

Geographic entities mentioned:
surface_form: San Gabriel Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.101944444444
lon: -118.10277777778
El Paso, La Palma. El Paso, also known as Ciudad de El Paso, is a Spanish municipality located on the island of La Palma, province of Santa Cruz de Tenerife, Canary Islands. Geographically it is located in the center of the island of La Palma, covering to the west with the Caldera de Taburiente, part of the Aridane Valley, the Cumbre Nueva and the Cumbre Vieja.

Geographic entities mentioned:
surface_form: Cumbre Vieja
instance_of: Mountain
countries: Spain
coordinates: lat: 28.566666666667
lon: -17.833333333333
Ibarra, Ecuador. Ibarra (; full name San Miguel de Ibarra; Quechua: Impapura) is a city in northern Ecuador and the capital of the Imbabura Province. It lies at the foot of the Imbabura Volcano and on the left bank of the Tahuando river. It is located about northeast of Ecuador's capital Quito. History.

Geographic entities mentioned:
surface_form: Imbabura Volcano
instance_of: Mountain
countries: Ecuador
coordinates: lat: 0.25805555555556
lon: -78.179722222222
The Inca ruler Atahualpa is said to have been born in the Inca settlement of Inca-Caranqui about 2 km from the city. Helados de paila (handmade ice cream or sorbet and still sold in the markets today) was first made in Ibarra during Incan times (but not by Incas; by the native indigenous), using snow or ice from the nearby Imbabura Volcano (which is no longer snow bound).

Geographic entities mentioned:
surface_form: Imbabura Volcano
instance_of: Mountain
countries: Ecuador
coordinates: lat: 0.25805555555556
lon: -78.179722222222
Lenglingen. Lenglingen is a lake in Lierne Municipality in Trøndelag county, Norway. The lake is fed by the lakes Holden and Gusvatnet, and the water from Lenglingen flows south into the lake Ulen. The village of Mebygda lies on the southeastern shore of the lake.

Geographic entities mentioned:
surface_form: Gusvatnet
instance_of: Lake
countries: Norway
coordinates: lat: 64.2825
lon: 13.4889
surface_form: lenglingen
instance_of: Lake
countries: Norway
coordinates: lat: 64.25
lon: 13.716666666667
Lenglingen. Lenglingen is a lake in Lierne Municipality in Trøndelag county, Norway. The lake is fed by the lakes Holden and Gusvatnet, and the water from Lenglingen flows south into the lake Ulen. The village of Mebygda lies on the southeastern shore of the lake.

Geographic entities mentioned:
surface_form: lenglingen
instance_of: Lake
countries: Norway
coordinates: lat: 64.25
lon: 13.716666666667
The mountain has no official trail. Geography. The Manitook Mountain ridgeline rises steeply to above the surrounding landscape, with several distinct summits and a high point of above sea level. Located entirely within Granby, Connecticut, its northern summit abuts the Connecticut/ Massachusetts border near Southwick, Massachusetts.

Geographic entities mentioned:
surface_form: high point
instance_of: Mountain
countries: United States
coordinates: lat: 41.924722222222
lon: -74.288055555556
surface_form: manitook mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.995
lon: -72.775833333333
surface_form: high point
instance_of: Mountain
countries: United States
coordinates: lat: 41.3209
lon: -74.6616
Manitook Mountain. Manitook Mountain, also called Manituck Mountain, is a long traprock mountain ridge located between the Berkshires and the Connecticut River Valley in north-central Connecticut.

Geographic entities mentioned:
surface_form: manitook mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.995
lon: -72.775833333333
Manitook Mountain. Manitook Mountain, also called Manituck Mountain, is a long traprock mountain ridge located between the Berkshires and the Connecticut River Valley in north-central Connecticut.

Geographic entities mentioned:
surface_form: manitook mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.995
lon: -72.775833333333
surface_form: river valley
instance_of: Valley
countries: United States
coordinates: lat: 35.36
lon: -93.37
It is an outlying ridge belonging to the narrow, linear Metacomet Ridge that extends from Long Island Sound near New Haven, Connecticut, north through the Connecticut River Valley of Massachusetts to the Vermont border. Manitook Mountain is known for its ledges and microclimate ecosystems. The mountain has no official trail. Geography.

Geographic entities mentioned:
surface_form: manitook mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.995
lon: -72.775833333333
Geology and ecology. Manitook Mountain, like much of the Metacomet Ridge, is composed of basalt, also called traprock, a volcanic rock. The mountain formed near the end of the Triassic Period with the rifting apart of the North American continent from Africa and Eurasia. Lava welled up from the rift and solidified into sheets of strata hundreds of feet thick.

Geographic entities mentioned:
surface_form: manitook mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.995
lon: -72.775833333333
The mountain formed near the end of the Triassic Period with the rifting apart of the North American continent from Africa and Eurasia. Lava welled up from the rift and solidified into sheets of strata hundreds of feet thick. Subsequent faulting and earthquake activity tilted the strata, creating the cliffs and ridgeline of Manitook Mountain.

Geographic entities mentioned:
surface_form: manitook mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.995
lon: -72.775833333333
Hot, dry upper slopes, cool, moist ravines, and mineral-rich ledges of basalt talus produce a combination of microclimate ecosystems on the mountain that support plant and animal species uncommon in greater Connecticut. Manitook Mountain is also an important raptor migration path. (See Metacomet Ridge for more information on the geology and ecosystem of Manitook Mountain).

Geographic entities mentioned:
surface_form: manitook mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.995
lon: -72.775833333333
Manitook Mountain is also an important raptor migration path. (See Metacomet Ridge for more information on the geology and ecosystem of Manitook Mountain). Conservation and recreation. Expanding suburban sprawl presents the greatest threats to the unique ecosystem and landscape of Manitook Mountain. As of 2007, much of the mountain was still wooded and undeveloped.

Geographic entities mentioned:
surface_form: manitook mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.995
lon: -72.775833333333
(See Metacomet Ridge for more information on the geology and ecosystem of Manitook Mountain). Conservation and recreation. Expanding suburban sprawl presents the greatest threats to the unique ecosystem and landscape of Manitook Mountain. As of 2007, much of the mountain was still wooded and undeveloped. The Granby Land Trust manages several properties on and near the mountain.

Geographic entities mentioned:
surface_form: manitook mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.995
lon: -72.775833333333
Manitook Mountain, also called Manituck Mountain, is a long traprock mountain ridge located between the Berkshires and the Connecticut River Valley in north-central Connecticut. It is an outlying ridge belonging to the narrow, linear Metacomet Ridge that extends from Long Island Sound near New Haven, Connecticut, north through the Connecticut River Valley of Massachusetts to the Vermont border.

Geographic entities mentioned:
surface_form: long island
instance_of: Landform
countries: United States
coordinates: lat: 46.7269
lon: -90.785
surface_form: river valley
instance_of: Valley
countries: United States
coordinates: lat: 35.36
lon: -93.37
The mountain is particularly prominent as viewed from the Congamond Lakes to the north. The north side of the mountain drains into the Congamond Lakes then into Great Brook, thence to the Westfield River, the Connecticut River, and Long Island Sound. The remainder of the mountain is of the Salmon Brook watershed, which drains into the Farmington River, thence into the Connecticut River.

Geographic entities mentioned:
surface_form: long island
instance_of: Landform
countries: United States
coordinates: lat: 46.7269
lon: -90.785
Demography. Native Goan Muslims are concentrated in the Novas Conquistas regions of Sattari, Bicholim, Sanguem, Ponda, Betul, Salcete, Tiswadi, Canacona, Pilar, Old Goa, Bardez and some areas of the coast of Vasco Da Gama. Their language parallels Dakhini of the Deccan Plateau. This dialect of Urdu has heavy Konkani influence and may be considered the &quot;Konkani slang&quot; of Goan Muslims.

Geographic entities mentioned:
surface_form: Deccan Plateau
instance_of: Plateau
countries: India
coordinates: lat: 15
lon: 77
The horse would be led over the hill and the boat would be propelled by legging. The term &quot;canal tunnel&quot; is not commonly applied to tunnels used to conduct water (for irrigation, water supply, etc.), such as the 48-kilometre-long Arpa-Sevan tunnel in Armenia (see List of longest tunnels), or a number of tunnels on the Irtysh–Karamay–Ürümqi Canal in China.

Geographic entities mentioned:
surface_form: Sevan
instance_of: Lake
countries: Armenia
coordinates: lat: 40.310555555556
lon: 45.349166666667
Mount Hosmer (British Columbia). Mount Hosmer is a mountain of the Canadian Rockies in British Columbia, Canada. It shares its name with the adjacent community of Hosmer, but its best-known elevation, a series of south-facing cliffs, can be seen from further down the Elk Valley in Fernie.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: mount hosmer (british columbia)
instance_of: Mountain
countries: Canada
coordinates: lat: 49.61388888888889
lon: -115.01138888888889
Mount Hosmer (British Columbia). Mount Hosmer is a mountain of the Canadian Rockies in British Columbia, Canada. It shares its name with the adjacent community of Hosmer, but its best-known elevation, a series of south-facing cliffs, can be seen from further down the Elk Valley in Fernie.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: mount hosmer
instance_of: Mountain
countries: Canada
coordinates: lat: 49.61388888888889
lon: -115.01138888888889
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Mount Hosmer is a mountain of the Canadian Rockies in British Columbia, Canada. It shares its name with the adjacent community of Hosmer, but its best-known elevation, a series of south-facing cliffs, can be seen from further down the Elk Valley in Fernie. The mountain is an upside down mountain, where the oldest part of the rock formation is near the top and the youngest is at the bottom.

Geographic entities mentioned:
surface_form: elk valley
instance_of: Valley
countries: Canada
coordinates: lat: 49.546
lon: -115.005