Sarmila/GeoWiki-Features huggingface dataset:
A short unnamed creek flows in at the north. The primary outflow, at the south, is an unnamed creek towards Lost Lake, which flows via Calcite Creek, Sydney Creek and the Montreal River to Lake Timiskaming on the Ottawa River. A second Crawford Lake in Timiskaming District and also in the same drainage basins, Crawford Lake (Milner Township), lies just southwest.

Geographic entities mentioned:
surface_form: crawford lake
instance_of: Lake
countries: Canada
coordinates: lat: 48.0908
lon: -91.2892
surface_form: crawford lake
instance_of: Lake
countries: Canada
coordinates: lat: 48.0908
lon: -91.2892
surface_form: crawford lake
instance_of: Lake
countries: Canada
coordinates: lat: 47.7008
lon: -80.6828
surface_form: crawford lake
instance_of: Lake
countries: Canada
coordinates: lat: 47.7008
lon: -80.6828
surface_form: crawford lake
instance_of: Lake
countries: Canada
coordinates: lat: 48.1394
lon: -81.9683
surface_form: crawford lake
instance_of: Lake
countries: Canada
coordinates: lat: 48.1394
lon: -81.9683
Wugai Mountain. Wugai Mountain () is located in the Chenzhou area of Hunan province in China. It reaches 1600 metres above sea level. It is the location of Wugai Mountain Hunting Field. Among the types of animals that live in the dense woods that cover the mountain are sambar, wild boar and chamois.

Geographic entities mentioned:
surface_form: wugai mountain
instance_of: Mountain
countries: People's Republic of China
The lake basin is well defined, located in the ancient valley of the Kasmala River. A southern branch at the head of the Kasmala flows out of the lake. The northern end of lake Gorkoye (Chernokurynskoye) is located to the southwest and lake Gorkoye (Romanovsky District) slightly to the WNW. Lake Zerkalnoye lies to the southeast and Mostovoye to the northwest. Flora and fauna.

Geographic entities mentioned:
surface_form: chernokurynskoye
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 52.47485
lon: 81.325123
surface_form: gorkoye (chernokurynskoye)
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 52.47485
lon: 81.325123
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
Bolshoye Ostrovnoye. Bolshoye Ostrovnoye () is a salt lake in Mamontovsky District, Altai Krai, Russian Federation. The lake lies roughly in the middle of the Krai. Mamontovo, Ostrovnoye and Malye Butyrki are located close to the lakeshore. The nearest towns are Bukanskoye, near the northern end, and Kazantsevo to the southwest. Geography.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
surface_form: bolshoye ostrovnoye
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 52.725594444444
lon: 81.704816666667
Bolshoye Ostrovnoye. Bolshoye Ostrovnoye () is a salt lake in Mamontovsky District, Altai Krai, Russian Federation. The lake lies roughly in the middle of the Krai. Mamontovo, Ostrovnoye and Malye Butyrki are located close to the lakeshore. The nearest towns are Bukanskoye, near the northern end, and Kazantsevo to the southwest. Geography.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
The nearest towns are Bukanskoye, near the northern end, and Kazantsevo to the southwest. Geography. Bolshoye Ostrovnoye is an endorheic lake that lies within one of the wide ravines of glacial origin cutting diagonally across the Ob Plateau. The lake has an irregular shape, stretching roughly from northeast to southwest for over.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
surface_form: bolshoye ostrovnoye
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 52.725594444444
lon: 81.704816666667
Geography. Bolshoye Ostrovnoye is an endorheic lake that lies within one of the wide ravines of glacial origin cutting diagonally across the Ob Plateau. The lake has an irregular shape, stretching roughly from northeast to southwest for over. It has a very narrow southern section, and the broader section has two opposing landspits in the middle that almost divide the lake in two.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
The lake has an irregular shape, stretching roughly from northeast to southwest for over. It has a very narrow southern section, and the broader section has two opposing landspits in the middle that almost divide the lake in two. There is an island near the northern shore. The bottom of the lake is sandy and most of the shore is low and swampy.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
It has a very narrow southern section, and the broader section has two opposing landspits in the middle that almost divide the lake in two. There is an island near the northern shore. The bottom of the lake is sandy and most of the shore is low and swampy. The lake basin is well defined, located in the ancient valley of the Kasmala River.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
There is an island near the northern shore. The bottom of the lake is sandy and most of the shore is low and swampy. The lake basin is well defined, located in the ancient valley of the Kasmala River. A southern branch at the head of the Kasmala flows out of the lake.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
The bottom of the lake is sandy and most of the shore is low and swampy. The lake basin is well defined, located in the ancient valley of the Kasmala River. A southern branch at the head of the Kasmala flows out of the lake. The northern end of lake Gorkoye (Chernokurynskoye) is located to the southwest and lake Gorkoye (Romanovsky District) slightly to the WNW.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
A southern branch at the head of the Kasmala flows out of the lake. The northern end of lake Gorkoye (Chernokurynskoye) is located to the southwest and lake Gorkoye (Romanovsky District) slightly to the WNW. Lake Zerkalnoye lies to the southeast and Mostovoye to the northwest. Flora and fauna. The ribbon pine forest characteristic of the Ob Plateau flanks the eastern side of Bolshoye Ostrovnoye.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
The ribbon pine forest characteristic of the Ob Plateau flanks the eastern side of Bolshoye Ostrovnoye. Bulrushes and willows grow by the shore. The water is only slightly saline and fish were once abundant in the lake. Pike, crucian carp and roach are still to be found in its waters, however, in recent decades species such as tench, peled and perch have disappeared owing to eutrophication.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
The water is only slightly saline and fish were once abundant in the lake. Pike, crucian carp and roach are still to be found in its waters, however, in recent decades species such as tench, peled and perch have disappeared owing to eutrophication. At the time of the USSR there used to be a fish processing plant by the lakeshore, where fish caught in the lake was smoked.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
At the time of the USSR there used to be a fish processing plant by the lakeshore, where fish caught in the lake was smoked. The facility was abandoned about 25 years ago, but currently there are plans to revive it and stock the lake with fish.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
Bolshoye Ostrovnoye. Bolshoye Ostrovnoye () is a salt lake in Mamontovsky District, Altai Krai, Russian Federation. The lake lies roughly in the middle of the Krai. Mamontovo, Ostrovnoye and Malye Butyrki are located close to the lakeshore. The nearest towns are Bukanskoye, near the northern end, and Kazantsevo to the southwest. Geography.

Geographic entities mentioned:
surface_form: bolshoye ostrovnoye
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 52.725594444444
lon: 81.704816666667
Lake Zerkalnoye lies to the southeast and Mostovoye to the northwest. Flora and fauna. The ribbon pine forest characteristic of the Ob Plateau flanks the eastern side of Bolshoye Ostrovnoye. Bulrushes and willows grow by the shore. The water is only slightly saline and fish were once abundant in the lake.

Geographic entities mentioned:
surface_form: bolshoye ostrovnoye
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 52.725594444444
lon: 81.704816666667
Flatters temporarily resolved the problem by relieving Le Chatelier of his command. The mission reached Lake Menghough on the fringe of the Tuareg of the Ajjer country, then returned in May 1880. When the second Flatters expedition was being organized later in 1880 Le Chatelier was among the members of the first expedition who asked for other assignments.

Geographic entities mentioned:
surface_form: Lake Menghough
instance_of: Lake
countries: Algeria
France
coordinates: lat: 26.382478
lon: 8.817555
Kebnekaise mountain lodge. Kebnekaise mountain lodge (Kebnekaise fjällstation), elevation, is situated at the base of Mount Kebnekaise, west of Nikkaluokta, which in turn is situated west of Kiruna in Lappland, Sweden. The lodge is owned and managed by the Swedish Tourist Association (STF). Facilities.

Geographic entities mentioned:
surface_form: Kebnekaise
instance_of: Mountain
countries: Sweden
coordinates: lat: 67.883333333333
lon: 18.55
The lodge offers guided tours to the summit of Kebnekaise. The ascent takes roughly 10-12 hours. The road ends at Nikkaluokta and from there on one has to walk. The walk from Nikkaluokta to Kebnekaise takes approximately 6 h. After there is a restaurant called &quot;Enoks&quot; by the lake Ladtjojaure. It is also possible to take a helicopter from Nikkaluokta to the Kebnekaise Mountain lodge.

Geographic entities mentioned:
surface_form: Kebnekaise
instance_of: Mountain
countries: Sweden
coordinates: lat: 67.883333333333
lon: 18.55
In 1883, prospectors discovered a rich vein of colemanite borax in the Calico Mountains 4 miles east from the silver mining town of Calico. The claim was bought by mining tycoon William Tell Coleman, who owned and worked several borax mines in Death Valley, including the Harmony Borax Works, famous for the Twenty-mule teams which were used to haul borax to the railroads at Mojave, California.

Geographic entities mentioned:
surface_form: Twenty-mule team
instance_of: Valley
countries: United States
At first, twenty-mule teams had been used to haul the borax to the railhead at Daggett, California, but Smith was not happy with the cost and upkeep with the mules and wagons, and in 1894, made efforts to replace them with a Daniel Best steam tractor (now called &quot;Old Dinah&quot;) which was not well equipped for running in the desert.

Geographic entities mentioned:
surface_form: twenty-mule team
instance_of: Valley
countries: United States
Ardpatrick, County Limerick. Ardpatrick () is a small village in County Limerick, Ireland. It lies at the foot of the north slopes of the Ballyhoura Mountains, on the edge of the Golden Vale. As of the 2006 census, the electoral division of Ardpatrick which contains the village, had a population of 398.

Geographic entities mentioned:
surface_form: Golden Vale
instance_of: Valley
countries: Ireland
coordinates: lat: 52.4
lon: -8.4
Restoule. Restoule is a community and designated place in geographic Patterson Township in the Centre Unorganized Part of Parry Sound District in Central Ontario, Canada. It is situated on the Restoule River between Commanda Lake, and Restoule Lake and is part of the Almaguin Highlands region.

Geographic entities mentioned:
surface_form: Commanda Lake
instance_of: Lake
countries: Canada
coordinates: lat: 46.0167
lon: -79.7
surface_form: Restoule Lake
instance_of: Lake
countries: Canada
coordinates: lat: 46.05
lon: -79.7667
Along with the nearby communities of Loring and Port Loring and other smaller hamlets, the area promotes itself as the Loring-Restoule tourist area. Restoule is located south of Lake Nipissing, and north of Ontario's famous cottage country. Despite being north of this area, Restoule is a major centre for cottages, as is the entire Loring-Restoule region.

Geographic entities mentioned:
surface_form: Lake Nipissing
instance_of: Lake
countries: Canada
coordinates: lat: 46.283333333333
lon: -80
Yangebup Lake. Yangebup Lake is a freshwater lake in the suburb of Yangebup, south-west of the central business district of Perth, the capital of Western Australia. It is part of Beeliar Regional Park. Overview. Yangebup Lake's name is derived from the Noongar word for the locally-growing bullrush (&quot;Typha domingensis&quot;), &quot;yanget&quot;.

Geographic entities mentioned:
surface_form: yangebup lake
instance_of: Lake
countries: Australia
coordinates: lat: -32.118333333333
lon: 115.83
It is part of Beeliar Regional Park. Overview. Yangebup Lake's name is derived from the Noongar word for the locally-growing bullrush (&quot;Typha domingensis&quot;), &quot;yanget&quot;. The lake and its name were first recorded by European settlers in 1841 while the suburb of Yangebup officially received its name in 1977.

Geographic entities mentioned:
surface_form: yangebup lake
instance_of: Lake
countries: Australia
coordinates: lat: -32.118333333333
lon: 115.83
The plan had four main routes from the bridge towards the city center, and the bridge was planned with two clearances. The first alternative involved a tunnel from the bridge to Gravdalsvatnet, which would be the shortest route.

Geographic entities mentioned:
surface_form: Gravdalsvatnet
instance_of: Lake
countries: Norway
coordinates: lat: 60.381
lon: 5.263
Alternative three involved the tunnel running southwards and intersecting with 555 at Loddefjord. Alternative four involved an even more western route, and would intersect at Storavatnet. Alternative four gave a longer route to the city center than alternative one, but was regarded as the best technically and with the least environmental impact. The agency recommended the first or fourth proposal.

Geographic entities mentioned:
surface_form: Storavatnet
instance_of: Lake
countries: Norway
coordinates: lat: 60.362
lon: 5.215
In 1908 Mander visited his uncle Martin Mander in New Zealand and for a short period took up sheep farming on his uncle's station. Martin Mander had emigrated to New Zealand in 1890 and established the 'Horoeka-Waimata' sheep station in the Waimata Valley, near Gisborne on the north-east coast of New Zealand's North Island. In early 1909 Lionel Mander lived briefly in Australia.

Geographic entities mentioned:
surface_form: Waimata Valley
instance_of: Valley
countries: New Zealand
coordinates: lat: -38.5042
lon: 178.0566
Route 30 northwest of Portland. Cornelius Pass is one of only two main north–south connecting roads in Hillsboro. By 2006, the former country road handled 11,000 drivers each day, though it was designed for 10,000, because it is an arterial route from the Tualatin Valley between Hillsboro to the Columbia River north of Portland; 1,500 of the 11,000 vehicles were tractor-trailers.

Geographic entities mentioned:
surface_form: Tualatin Valley
instance_of: Valley
countries: United States
coordinates: lat: 45.5106
lon: -122.989
History. Andrew Murray Vineyards was founded in 1990 when entrepreneurs Jim and Fran Murray sold their southern California restaurants and 'retired' to 200 acres of fertile soil in the Santa Ynez Valley. With their son and winemaker Andrew Murray at the helm, the Los Olivos winery is now a well-respected purveyor of Rhône-style wines.

Geographic entities mentioned:
surface_form: Santa Ynez Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.5473
lon: -119.858
It is set on the northern boundary of Shey Phoksundo National Park. Precipitation runoff from the mountain's southern slopes drains into tributaries of the Karnali River, whereas the northern slope drains into the Maquan River drainage basin of Tibet. Topographic relief is significant as the summit rises 1,660 metres (5,446 ft) in along the southwest slope.

Geographic entities mentioned:
surface_form: Maquan River
instance_of: Watercourse
countries: People's Republic of China
coordinates: lat: 29.6
lon: 84.15
Kubi Gangri. Kaqur Kangri, also known as Kanti Himal or Kubi Kangri, is a mountain in Nepal and China. Description. Kaqur Kangri is a mountain in the Himalayas of Asia. It has a summit elevation of 6,859 meters above sea level and is located on the international border between Nepal and Tibet, China. It is set on the northern boundary of Shey Phoksundo National Park.

Geographic entities mentioned:
surface_form: kaqur kangri
instance_of: Mountain
countries: Nepal
coordinates: lat: 29.7658
lon: 82.7517
Climate. Based on the Köppen climate classification, Kaqur Kangri is located in a tundra climate zone with cold, snowy winters, and cool summers. Weather systems are forced upwards by the Himalaya mountains (orographic lift), causing heavy precipitation in the form of rainfall and snowfall. Mid-June through early-August is the monsoon season.

Geographic entities mentioned:
surface_form: kaqur kangri
instance_of: Mountain
countries: Nepal
coordinates: lat: 29.7658
lon: 82.7517
Kubi Gangri. Kaqur Kangri, also known as Kanti Himal or Kubi Kangri, is a mountain in Nepal and China. Description. Kaqur Kangri is a mountain in the Himalayas of Asia. It has a summit elevation of 6,859 meters above sea level and is located on the international border between Nepal and Tibet, China. It is set on the northern boundary of Shey Phoksundo National Park.

Geographic entities mentioned:
surface_form: kubi gangri
instance_of: Mountain
countries: Nepal
coordinates: lat: 29.7658
lon: 82.7517
USCGC &quot;Mohawk&quot; (WMEC-913) is a 270' United States Coast Guard Famous-class medium endurance cutter. She was launched on September 9, 1989 at Robert Derecktor Shipyard Incorporated of Middletown, Rhode Island and commissioned in March 1991. She is the third cutter named for the Mohawk nation, a tribe of Iroquoian Indians from the Mohawk Valley of New York. Service history.

Geographic entities mentioned:
surface_form: Mohawk Valley
instance_of: Valley
countries: United States
Eiði Power Plant. The Eiði Hydroelectric Power Station () is the largest hydroelectric power station in the Faroe Islands. It stands below a dam on Lake Eiði (elevation) on the island of Eysturoy. The power plant started production on April 28, 1987, and it was built and is owned by the power producer and distributor SEV. Originally, two Francis turbines were installed with a capacity of each.

Geographic entities mentioned:
surface_form: Lake Eiði
instance_of: Lake
countries: Faroe Islands
coordinates: lat: 62.28611111
lon: -7.05277778
By October 2018, Diwata-1 has captured 14,492 images in the Philippines covering an area equivalent to 32 percent of the country's land area. Among those captured images was that of Semirara Island and Laguna de Bay. As of the same month, the satellite remained operational and was projected to be still functioning for at least three years given favorable conditions in space.

Geographic entities mentioned:
surface_form: Laguna de Bay
instance_of: Lake
countries: Philippines
coordinates: lat: 14.508888888889
lon: 121.11888888889
Geography. Located immediately to the south-west of Cam Loch, and at a slightly lower level, is Loch Veyatie, which is roughly parallel to it. The two lochs are connected by Abhainn Mhòr, which consists of extensions of the two lochs with a waterfall between them. It is an area that holds several large lochs, for example the irregular-shaped Loch Sionascaig, directly to the west.

Geographic entities mentioned:
surface_form: Loch Veyatie
instance_of: Lake
countries: United Kingdom
coordinates: lat: 58.075
lon: -5.0888888888889
surface_form: loch veyatie
instance_of: Lake
countries: United Kingdom
coordinates: lat: 58.075
lon: -5.0888888888889
surface_form: cam loch
instance_of: Lake
countries: United Kingdom
coordinates: lat: 58.075157
lon: -5.032002
The two lochs are connected by Abhainn Mhòr, which consists of extensions of the two lochs with a waterfall between them. It is an area that holds several large lochs, for example the irregular-shaped Loch Sionascaig, directly to the west. The loch is overlooked by the twin peaks of Cùl Mòr at 849m to the south-west. Directly south of the loch is Canisp at 847m.

Geographic entities mentioned:
surface_form: Loch Sionascaig
instance_of: Lake
countries: United Kingdom
coordinates: lat: 58.066666666667
lon: -5.1833333333333
The two lochs are connected by Abhainn Mhòr, which consists of extensions of the two lochs with a waterfall between them. It is an area that holds several large lochs, for example the irregular-shaped Loch Sionascaig, directly to the west. The loch is overlooked by the twin peaks of Cùl Mòr at 849m to the south-west. Directly south of the loch is Canisp at 847m.

Geographic entities mentioned:
surface_form: Cùl Mòr
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 58.057980555556
lon: -5.1168
surface_form: cùl mòr
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 58.057980555556
lon: -5.1168
It is an area that holds several large lochs, for example the irregular-shaped Loch Sionascaig, directly to the west. The loch is overlooked by the twin peaks of Cùl Mòr at 849m to the south-west. Directly south of the loch is Canisp at 847m. To the south-east, is the steep-sides ridge that forms the mountain of Suilven at 723m.

Geographic entities mentioned:
surface_form: Canisp
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 58.12125
lon: -5.0521
The loch is overlooked by the twin peaks of Cùl Mòr at 849m to the south-west. Directly south of the loch is Canisp at 847m. To the south-east, is the steep-sides ridge that forms the mountain of Suilven at 723m. Cam Loch sits in an area of wilderness landscape of moorland, bogs, and lochs and lochans. Cam Loch is fed by inflows from Loch Urigill and Loch Borralan via the River Ledbeg.

Geographic entities mentioned:
surface_form: Suilven
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 58.115
lon: -5.1370694444444
surface_form: suilven
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 58.115
lon: -5.1370694444444
Cam Loch sits in an area of wilderness landscape of moorland, bogs, and lochs and lochans. Cam Loch is fed by inflows from Loch Urigill and Loch Borralan via the River Ledbeg. The loch drains via Abhainn Mhòr, into Loch Veyatie, that is part of the Fionn Loch Drainage System, that drains into Fionn Loch, that in turn is drained by the River Kirkaig into the sea. Interglacial site.

Geographic entities mentioned:
surface_form: Loch Urigill
instance_of: Lake
countries: United Kingdom
coordinates: lat: 58.033333333333
lon: -4.9666666666667
surface_form: Loch Borralan
instance_of: Lake
countries: United Kingdom
coordinates: lat: 58.05
lon: -4.9333333333333
Cam Loch sits in an area of wilderness landscape of moorland, bogs, and lochs and lochans. Cam Loch is fed by inflows from Loch Urigill and Loch Borralan via the River Ledbeg. The loch drains via Abhainn Mhòr, into Loch Veyatie, that is part of the Fionn Loch Drainage System, that drains into Fionn Loch, that in turn is drained by the River Kirkaig into the sea. Interglacial site.

Geographic entities mentioned:
surface_form: loch veyatie
instance_of: Lake
countries: United Kingdom
coordinates: lat: 58.075
lon: -5.0888888888889
Cam Loch, Sutherland. Cam Loch (the crooked loch) is an irregularly-shaped freshwater loch, about 5 km long, on a north-west to south-east orientation, located slightly north of the village of Elphin, in the Assynt district of Sutherland, Scotland.

Geographic entities mentioned:
surface_form: cam loch, sutherland
instance_of: Lake
countries: United Kingdom
coordinates: lat: 58.075157
lon: -5.032002
Cam Loch, Sutherland. Cam Loch (the crooked loch) is an irregularly-shaped freshwater loch, about 5 km long, on a north-west to south-east orientation, located slightly north of the village of Elphin, in the Assynt district of Sutherland, Scotland.

Geographic entities mentioned:
surface_form: cam loch
instance_of: Lake
countries: United Kingdom
coordinates: lat: 58.075157
lon: -5.032002
The loch is overlooked by the twin peaks of Cùl Mòr at 849m to the south-west. Directly south of the loch is Canisp at 847m. To the south-east, is the steep-sides ridge that forms the mountain of Suilven at 723m. Cam Loch sits in an area of wilderness landscape of moorland, bogs, and lochs and lochans. Cam Loch is fed by inflows from Loch Urigill and Loch Borralan via the River Ledbeg.

Geographic entities mentioned:
surface_form: cam loch
instance_of: Lake
countries: United Kingdom
coordinates: lat: 58.075157
lon: -5.032002
Imboden's and William L. Jackson's Brigade and after the participating in the Gettysburg Campaign, skirmished the Federals in western Virginia. Later it served in the Shenandoah Valley, participating in the Battle of New Market in 1864, and disbanded during April, 1865. The field officers were Colonel George W. Imboden (brother of John D.), Lieutenant Colonel David E. Beall, and Major Alexander W.

Geographic entities mentioned:
surface_form: Shenandoah Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.5
lon: -78.85
The Qualla Boundary, which is the reserve of the Eastern Band of Cherokee Indians, includes parts of the range's northwest section along Soco Creek. Waterrock Knob, which has an elevation of, is the highest summit in the Plott Balsams. Four other summits in the range rise above 6,000 feet, namely Mount Lyn Lowry, Browning Knob, Plott Balsam Mountain, and Yellow Face.

Geographic entities mentioned:
surface_form: Waterrock Knob
instance_of: Mountain
countries: United States
coordinates: lat: 35.464269444444
lon: -83.137644444444
Orustdalen. Orustdalen is a valley in Nordenskiöld Land at Spitsbergen, Svalbard. It is named after Swedish island of Orust in the province of Bohuslän. The valley has a length of about five kilometers and a width of two kilometers. It is located south of the mountains of Qvigstadfjellet, Christensenfjella and Systemafjellet.

Geographic entities mentioned:
surface_form: Qvigstadfjellet
instance_of: Mountain
countries: Norway
coordinates: lat: 77.956
lon: 14.054
surface_form: Christensenfjella
instance_of: Mountain
countries: Norway
coordinates: lat: 77.963
lon: 13.973
surface_form: Systemafjellet
instance_of: Mountain
countries: Norway
coordinates: lat: 77.9482
lon: 13.8956
Orustdalen. Orustdalen is a valley in Nordenskiöld Land at Spitsbergen, Svalbard. It is named after Swedish island of Orust in the province of Bohuslän. The valley has a length of about five kilometers and a width of two kilometers. It is located south of the mountains of Qvigstadfjellet, Christensenfjella and Systemafjellet.

Geographic entities mentioned:
surface_form: orustdalen
instance_of: Valley
countries: Norway
coordinates: lat: 77.936
lon: 13.96
Lake Bryan, Texas. Lake Bryan is a census-designated place (CDP) in Brazos County, Texas, United States, situated around a reservoir of the same name managed by Bryan Texas Utilities. The population was 2,060 at the 2020 census. It is part of the Bryan–College Station metropolitan area. Geography. Lake Bryan is located along the northwestern border of Brazos County.

Geographic entities mentioned:
surface_form: same name
instance_of: Lake
countries: United States
coordinates: lat: 30.712666666667
lon: -96.465833333333
Its southern terminus is at the LaSalle Expressway on the east bank of the Niagara River in Niagara Falls. The northern terminus is at New York State Route 18 (NY 18) at Four Mile Creek State Park in Porter near Lake Ontario. Originally, the parkway was one continuous road; however, due to low usage, a portion of the parkway near Niagara Falls was removed, separating the parkway into two sections.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
The parkway has entrance ramps from I-190 via Upper Mountain Road before passing under the bridge and becoming to a four-lane freeway again. Just north of the bridge, the Niagara Scenic Parkway approaches the edge of the Niagara Escarpment. Here, it is possible to see for several miles in any direction.

Geographic entities mentioned:
surface_form: Niagara Escarpment
instance_of: Mountain
countries: Canada
coordinates: lat: 43.8334
lon: -79.99966
Just north of the bridge, the Niagara Scenic Parkway approaches the edge of the Niagara Escarpment. Here, it is possible to see for several miles in any direction. Looking north, the remainder of the Niagara River can be seen, as can its mouth at Lake Ontario. The parkway descends the escarpment and meets NY 18F and NY 104 just east of the village of Lewiston.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
Albert Park Circuit. The Albert Park Circuit is a motorsport street circuit around Albert Park Lake in the suburb of Albert Park in Melbourne. It is used annually as a circuit for the Formula One Australian Grand Prix, the supporting Supercars Championship Melbourne SuperSprint and other associated support races. The circuit has an FIA Grade 1 licence.

Geographic entities mentioned:
surface_form: Albert Park Lake
instance_of: Lake
countries: Australia
coordinates: lat: -37.846
lon: 144.97
Santuario di Santa Rosalia, Palermo. The Sanctuary of Santa Rosalia is a church and pilgrimage site located on via Bonnaojust outside of the urban neighborhoods of Palermo, nestled against a stone cliff wall on Mount Pellegrino, which looms to the north of the Sicily city.

Geographic entities mentioned:
surface_form: Mount Pellegrino
instance_of: Mountain
countries: Italy
coordinates: lat: 38.17
lon: 13.351388888889
Thomas Ayres (artist). Thomas Almond Ayres (c. 1816-1858) was a California gold rush-era artist, most famous for drawing the first rendering of Yosemite Valley to be published and popularized. Ayres was born in Woodbridge, New Jersey in 1816. As a young adult, he moved to Wisconsin Territory and worked as a draftsman in what was to become St.

Geographic entities mentioned:
surface_form: Yosemite Valley
instance_of: Valley
countries: United States
coordinates: lat: 37.721694444444445
lon: -119.646
In the winter of 1857–1858, after stopping over in San Francisco, Ayres traveled around southern California gathering material. On April 26, 1858, as he was headed back to San Francisco, the passenger ship he was in sunk in a storm off Point Dume. Everyone on the ship perished, and all of the sketches Ayres had brought with him were lost.

Geographic entities mentioned:
surface_form: Point Dume
instance_of: Mountain
countries: United States
coordinates: lat: 34.001666666667
lon: -118.80611111111
Dévoluy Mountains. The Dévoluy Mountains (,) is a limestone massif located in Hautes-Alpes, France. It is part of the Dauphiné Prealps and is bordered by the Drac River to the north and the Buëch River to the south and west and is a popular destination for hiking, mountaineering and skiing. Its most notable peaks are the Grande Tête de l'Obiou (2,789 m) and Pic de Bure at 2,709 m.

Geographic entities mentioned:
surface_form: Grande Tête de l'Obiou
instance_of: Mountain
countries: France
coordinates: lat: 44.775
lon: 5.83972222
surface_form: Pic de Bure
instance_of: Mountain
countries: France
coordinates: lat: 44.6269
lon: 5.935
KV47. Tomb KV47, located in the Valley of the Kings in Egypt, was used for the burial of Pharaoh Siptah of the Nineteenth Dynasty. It was discovered on December 18, 1905 by Edward R. Ayrton, excavating on behalf of Theodore M. Davis; Siptah's mummy had been found earlier, cached in KV35. It was the last of the Nineteenth and Twentieth Dynasty kings tombs to be uncovered in the Valley.

Geographic entities mentioned:
surface_form: Valley of the Kings
instance_of: Valley
countries: Egypt
coordinates: lat: 25.74025
lon: 32.602358
The hill is named after the Thracian king Cersobleptes, 359-341 BC. Location. The hill is located at which is on the northeast coast of McFarlane Strait, 3.9 km south of Hrabar Nunatak, and 3.4 km west of Lloyd Hill (Bulgarian topographic survey 05 and mapping in 2005 and 2009).

Geographic entities mentioned:
surface_form: McFarlane Strait
instance_of: Body of water
coordinates: lat: -62.5333
lon: -59.9167
surface_form: Hrabar Nunatak
instance_of: Mountain
coordinates: lat: -62.452916666667
lon: -59.960555555556
surface_form: Lloyd Hill
instance_of: Mountain
coordinates: lat: -62.4898
lon: -59.8905
Kerseblept Nunatak. Kerseblept Nunatak (Nunatak Kerseblept \'nu-na-tak ker-se-'blept\) is a rocky hill of elevation 90 m projecting from Yakoruda Glacier on Greenwich Island in the South Shetland Islands, Antarctica. The hill is named after the Thracian king Cersobleptes, 359-341 BC. Location.

Geographic entities mentioned:
surface_form: kerseblept nunatak
instance_of: Mountain
coordinates: lat: -62.487916666667
lon: -59.955
Kerseblept Nunatak. Kerseblept Nunatak (Nunatak Kerseblept \'nu-na-tak ker-se-'blept\) is a rocky hill of elevation 90 m projecting from Yakoruda Glacier on Greenwich Island in the South Shetland Islands, Antarctica. The hill is named after the Thracian king Cersobleptes, 359-341 BC. Location.

Geographic entities mentioned:
surface_form: kerseblept nunatak
instance_of: Mountain
coordinates: lat: -62.487916666667
lon: -59.955
surface_form: nunatak kerseblept
instance_of: Mountain
coordinates: lat: -62.487916666667
lon: -59.955
Other foreign branches are located in London, Phoenix and Chicago. History. Till 1826 AD, Assam Territory was ruled mainly by Kachari, Ahoms in the entirety of Brahmaputra Valley and Koch. In 1826, after the Treaty of Yandabo the administration of Assam was passed down to the British, till independence in 1947. Since then Assam has been an integral part of India.

Geographic entities mentioned:
surface_form: Brahmaputra Valley
instance_of: Valley
countries: India
coordinates: lat: 26.5983
lon: 92.4506
Frenchman Butte. Frenchman Butte is a butte located northeast of Lloydminster, is named after a Frenchman who was killed there by Indians in the 19th century. It is not known how or why this man was murdered. This was also the site of the Battle of Frenchman's Butte between Major-General Thomas Bland Strange and Cree Chief Big Bear during the North-West rebellion.

Geographic entities mentioned:
surface_form: frenchman butte
instance_of: Mountain
countries: Canada
coordinates: lat: 53.6272
lon: -109.576
It is not known how or why this man was murdered. This was also the site of the Battle of Frenchman's Butte between Major-General Thomas Bland Strange and Cree Chief Big Bear during the North-West rebellion. The site of the battle was designated a National Historic Site of Canada in 1929.

Geographic entities mentioned:
surface_form: bear
instance_of: Watercourse
countries: Canada
coordinates: lat: 56.2833
lon: -126.967
Kikuji develops an interest in Fumiko, asking himself if he sees her mother in her. When Kikuji returns from a trip to Lake Nojiri, Miss Kurimoto brings him the news that both Miss Inamura and Fumiko have married another man in his absence. He learns that her story was a lie when Fumiko rings him to inform him that she will start a job and move into a flat farther away from him.

Geographic entities mentioned:
surface_form: Lake Nojiri
instance_of: Lake
countries: Japan
coordinates: lat: 36.826388888888886
lon: 138.22194444444443
Powder Ridge is dominated by apple orchards and agricultural fields, and is traversed by Powder Hill Road; the ridge offers expansive views to the east over the Connecticut River Valley, and is a popular local scenic drive. The Metacomet Ridge continues north from Besek Mountain as Higby Mountain and south as Trimountain.

Geographic entities mentioned:
surface_form: Higby Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.55
lon: -72.74
surface_form: Trimountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.460277777778
lon: -72.736111111111
surface_form: besek mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.513430555556
lon: -72.745930555556
surface_form: besek mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.513430555556
lon: -72.745930555556
surface_form: trimountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.460277777778
lon: -72.736111111111
surface_form: higby mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.55
lon: -72.74
Downhill skiing, snowboarding, and snow tubing are offered at the Powder Ridge Ski Area. Fishing and boating are allowed on Black Pond. The mountain is traversed by the Mattabesett Trail (maintained by the Connecticut Forest and Park Association), which stretches from the northern end of Lamentation Mountain, south to Totoket Mountain and north again to the Connecticut River.

Geographic entities mentioned:
surface_form: Lamentation Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.574166666667
lon: -72.7625
surface_form: Totoket Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.41722222222222
lon: -72.70194444444445
surface_form: lamentation mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.574166666667
lon: -72.7625
surface_form: totoket mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.41722222222222
lon: -72.70194444444445
The Metacomet Ridge continues north from Besek Mountain as Higby Mountain and south as Trimountain. The east side of Besek Mountain drains into the Coginchaug River, thence to the Connecticut River and Long Island Sound; the southwest side drains into the Muddy River, thence into the Quinnipiac River and Long Island Sound; and the northwest side into Harbor Brook, thence into the Quinnipiac River.

Geographic entities mentioned:
surface_form: muddy river
instance_of: Watercourse
countries: United States
coordinates: lat: 36.737500000000004
lon: -114.74416666666667
surface_form: besek mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.513430555556
lon: -72.745930555556
surface_form: long island
instance_of: Landform
countries: United States
coordinates: lat: 46.7269
lon: -90.785
surface_form: long island
instance_of: Landform
countries: United States
coordinates: lat: 46.7269
lon: -90.785
Besek Mountain. Besek Mountain (Alternate spelling: Bessic Mountain) also known as Black Mountain, est., is a traprock mountain ridge located southeast of Meriden, Connecticut. It is part of 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: besek mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.513430555556
lon: -72.745930555556
It is part of 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. Besek Mountain is known for its long line of open cliffs, unique microclimate ecosystems, and rare plant communities.

Geographic entities mentioned:
surface_form: besek mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.513430555556
lon: -72.745930555556
According to the Connecticut Forest and Park Association, the word &quot;Besek&quot; is a corruption of &quot;Besett&quot;, a Native American word for &quot;black.&quot; Besek Mountain, long by wide, with a 200–300-foot (60–90 m) high continuous 3-mile (5 km) long cliffline visible for miles, is located in Meriden, Middlefield, and Wallingford, Connecticut; its lower southeast slope is located in Durham, Connecticut.

Geographic entities mentioned:
surface_form: besek mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.513430555556
lon: -72.745930555556
Powder Ridge Ski Area is located on the east side of the mountain and extends to the summit. The northeast side of the mountain is occupied by a housing development, which reaches to the ridgeline. Powder Ridge or Powder Hill, forms the lower, eastern tier of Besek Mountain beneath the ski area.

Geographic entities mentioned:
surface_form: besek mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.513430555556
lon: -72.745930555556
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 Besek Mountain.

Geographic entities mentioned:
surface_form: besek mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.513430555556
lon: -72.745930555556
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. Besek Mountain is also an important raptor migration path. (See Metacomet Ridge for more information on the geology and ecosystem of Besek Mountain). Conservation and Recreation.

Geographic entities mentioned:
surface_form: besek mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.513430555556
lon: -72.745930555556
A trailhead for the Mattabesett Trail on Besek Mountain is located just west of the junction of Connecticut Route 68 and Connecticut Route 157 in Reeds Gap between Trimountain and Besek Mountain, west of Durham center. Black Pond can be accessed via a small parking lot off East Main Street in Meriden, east of Connecticut Route 15.

Geographic entities mentioned:
surface_form: besek mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.513430555556
lon: -72.745930555556
surface_form: besek mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.513430555556
lon: -72.745930555556
surface_form: trimountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.460277777778
lon: -72.736111111111
In December 2007, the Powder Ridge Ski Area website indicated that the ski area was closed. In 2012, the ski park was sold to the owner of Brownstone Exploration & Discovery Park in nearby Portland, Connecticut, and was reopened as Powder Ridge Mountain Park & Resort in December 2013. Besek Mountain, its habitat, and access to its ridgeline are most threatened by potential development.

Geographic entities mentioned:
surface_form: besek mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.513430555556
lon: -72.745930555556
The and the are active conservation partners in the area. Historic events. The infamous aborted Powder Ridge Rock Festival was to be held on Besek Mountain July 30, August 1 and August 2, 1970 at Powder Ridge Ski Area.

Geographic entities mentioned:
surface_form: besek mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.513430555556
lon: -72.745930555556
Besek Mountain. Besek Mountain (Alternate spelling: Bessic Mountain) also known as Black Mountain, est., is a traprock mountain ridge located southeast of Meriden, Connecticut. It is part of 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
Black Pond can be accessed via a small parking lot off East Main Street in Meriden, east of Connecticut Route 15. The mountain may also be accessed via the parking area for Higby Mountain on Connecticut Route 66, just east of Black Pond, and via the ski slopes of the Powder Ridge Ski Area on Powder Hill Road in western Middlefield.

Geographic entities mentioned:
surface_form: higby mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.55
lon: -72.74
surface_form: black pond
instance_of: Lake
countries: United States
coordinates: lat: 43.1307
lon: -73.5616
surface_form: black pond
instance_of: Lake
countries: United States
coordinates: lat: 43.1307
lon: -73.5616
Powder Ridge or Powder Hill, forms the lower, eastern tier of Besek Mountain beneath the ski area. Powder Ridge is dominated by apple orchards and agricultural fields, and is traversed by Powder Hill Road; the ridge offers expansive views to the east over the Connecticut River Valley, and is a popular local scenic drive.

Geographic entities mentioned:
surface_form: river valley
instance_of: Valley
countries: United States
coordinates: lat: 35.36
lon: -93.37
Considered particularly scenic is Black Pond, located on the northwest side of the mountain. Cliffs and talus slopes plunge into the pond from the ridgeline. Other bodies of water on the mountain include the developed Besek Lake on the east side of the mountain, and the lower end of the Mount Higby Reservoir on the north side.

Geographic entities mentioned:
surface_form: black pond
instance_of: Lake
countries: United States
coordinates: lat: 43.1307
lon: -73.5616
Downhill skiing, snowboarding, and snow tubing are offered at the Powder Ridge Ski Area. Fishing and boating are allowed on Black Pond. The mountain is traversed by the Mattabesett Trail (maintained by the Connecticut Forest and Park Association), which stretches from the northern end of Lamentation Mountain, south to Totoket Mountain and north again to the Connecticut River.

Geographic entities mentioned:
surface_form: black pond
instance_of: Lake
countries: United States
coordinates: lat: 43.1307
lon: -73.5616
The mountain may also be accessed via the parking area for Higby Mountain on Connecticut Route 66, just east of Black Pond, and via the ski slopes of the Powder Ridge Ski Area on Powder Hill Road in western Middlefield. Black Pond, undeveloped and scenic, is part of the Black Pond Wildlife Management Area.

Geographic entities mentioned:
surface_form: black pond
instance_of: Lake
countries: United States
coordinates: lat: 43.1307
lon: -73.5616
Ilsestein. The Ilsestein (formerly also called &quot;Ilsenstein&quot;) is a prominent granite rock formation near the town of Ilsenburg in the Harz mountains of central Germany. Offering a scenic view over the Ilse valley to the Brocken massif, the highest mountain of the range, it is today a popular tourist destination. Geography.

Geographic entities mentioned:
surface_form: Ilse valley
instance_of: Valley
countries: Germany
coordinates: lat: 51.850277777778
lon: 10.666111111111
surface_form: Brocken
instance_of: Mountain
countries: Germany
Kingdom of Prussia
coordinates: lat: 51.800555555556
lon: 10.617222222222