Sarmila/GeoWiki-Features huggingface dataset:
Types. Macedonians wore 70 different types of national costumes, depending on the region where people lived, such as: Skopska Blatija, Skopska Crna Gora, Upper Polog, Lower Polog, Prilep-Bitola Plain, Upper Prespa, Lower Prespa, Ohrid Plain, Struga Plain, Drimkol, Malesija, Mariovo, Ovče Pole, Malesevo and many others.

Geographic entities mentioned:
surface_form: Skopska Crna Gora
instance_of: Mountain
countries: Serbia
Kosovo
North Macedonia
coordinates: lat: 42.166666666667
lon: 21.416666666667
The capital of the province is the city of Nakhon Ratchasima in Mueang Nakhon Ratchasima district, also called &quot;Khorat&quot;. Geography. The province is at the west end of the Khorat Plateau, separated from the Chao Phraya river valley by the Phetchabun and Dong Phaya Yen mountain ranges. Two national parks are in the province: Khao Yai in the west and Thap Lan in the south.

Geographic entities mentioned:
surface_form: Khorat Plateau
instance_of: Plateau
countries: Thailand
coordinates: lat: 15.666666666667
lon: 103.16666666667
The percentage of male population was 53.8% and the percentage of female population was 46.2%. Average Sex Ratio of Harike is 856 which is lower than Punjab state average of 895. Harike bird sanctuary. Harike barrage and Harike Wetland which are named after Harike village are located near this village. Migratory birds flock to this protected largest wetland in North India in winters.

Geographic entities mentioned:
surface_form: Harike Wetland
instance_of: Lake
countries: India
coordinates: lat: 31.15
lon: 74.96666666666667
With the establishment of the Bahmani Kingdom in the Deccan from 1347, the architectural styles of the Persian architecture of Iran made impressive and lasting impacts, which are seen in the Bidar Fort. The mosques, arches, gardens and the palaces were built within and also outside the fort in the Bidar city. Some of the important structures built are elaborated.

Geographic entities mentioned:
surface_form: Deccan
instance_of: Plateau
countries: India
coordinates: lat: 15
lon: 77
Bruno Malaguti. Bruno Malaguti (5 December 1887 – 2 December 1945) was an Italian general during World War II. Biography. After attending the Military Academy of Modena and graduating in 1909, Malaguti participated in the First World War with the rank of Second Lieutenant with the 5th Bersaglieri Regiment, fighting on the Col di Lana from 1915 to 1917.

Geographic entities mentioned:
surface_form: Col di Lana
instance_of: Mountain
countries: Italy
coordinates: lat: 46.49
lon: 11.97
The members of the Abihka were Upper Creek Indians. Their main place of residence was along the banks of the Upper Coosa and Alabama rivers, in what is now Talladega County, Alabama. Besides the town of Abihka, the Creek had established other important towns in their territory: &quot;Abihkutchi&quot;, &quot;Tuckabutche&quot;, &quot;Talladega&quot;, &quot;Coweta&quot;, and &quot;Kan-tcati&quot;.

Geographic entities mentioned:
surface_form: Coosa
instance_of: Watercourse
countries: United States
coordinates: lat: 32.4862464
lon: -86.2777475
Natore Raj and zamindari in Natore. In 1706 Raja Ramjivan Ray established his capital called &quot;Nator&quot; by filling the Chalan Beel. &quot;Nator&quot; meant 'stop the boat' as &quot;Nao&quot; meant boat and &quot;tharo&quot; meant stop. Natore was the headquarters of the British district of Rajshahi from 1769 to 1825 during colonial rule.

Geographic entities mentioned:
surface_form: Chalan Beel
instance_of: Lake
countries: Bangladesh
coordinates: lat: 24.52
lon: 89.01
In 1867 he published (&quot;Mount Athos and its monasteries&quot;), with a photo-lithographic reproduction of the geography of Ptolemy, of which the Greek manuscript of the 17th century is preserved in that monastery. He became a professor at the Collège de France in Paris.

Geographic entities mentioned:
surface_form: Mount Athos
instance_of: Mountain
countries: Greece
coordinates: lat: 40.15833333333333
lon: 24.327222222222222
Desolation Lava Field. The Desolation Lava Field (DLF) is a volcanic field at Mount Edziza in British Columbia, Canada. It reaches an elevation of on the Big Raven Plateau, but decreases to at Buckley Lake and in the Klastline River valley. The lava field covers more than and contains 10 volcanic cones that range in elevation from nearly.

Geographic entities mentioned:
surface_form: Mount Edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
Desolation Lava Field. The Desolation Lava Field (DLF) is a volcanic field at Mount Edziza in British Columbia, Canada. It reaches an elevation of on the Big Raven Plateau, but decreases to at Buckley Lake and in the Klastline River valley. The lava field covers more than and contains 10 volcanic cones that range in elevation from nearly.

Geographic entities mentioned:
surface_form: Big Raven Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.7167
lon: -130.75
The lava field covers more than and contains 10 volcanic cones that range in elevation from nearly. It is in Mount Edziza Provincial Park and is part of the Mount Edziza volcanic complex, the latter of which consists of several other volcanic landforms such as shield volcanoes, stratovolcanoes, lava domes and cinder cones.

Geographic entities mentioned:
surface_form: Mount Edziza volcanic complex
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5
lon: -130.6
The Triplex Cones were formed by subsequent eruptions and issued lava flows more than long. Renewed volcanism created Sidas Cone and Twin Cone, both of which differ from other cones in the Desolation Lava Field in that they are structurally complex. The younger Moraine Cone produced a roughly long lava flow that temporarily dammed the Klastline River and Kakiddi Creek.

Geographic entities mentioned:
surface_form: Sidas Cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.8589
lon: -130.628
The Triplex Cones were formed by subsequent eruptions and issued lava flows more than long. Renewed volcanism created Sidas Cone and Twin Cone, both of which differ from other cones in the Desolation Lava Field in that they are structurally complex. The younger Moraine Cone produced a roughly long lava flow that temporarily dammed the Klastline River and Kakiddi Creek.

Geographic entities mentioned:
surface_form: Kakiddi Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.872778
lon: -130.425556
The younger Moraine Cone produced a roughly long lava flow that temporarily dammed the Klastline River and Kakiddi Creek. Eve Cone and Williams Cone were produced by the latest eruptions in the Desolation Lava Field, the latter of which issued a long lava flow that temporarily dammed the Klastline River.

Geographic entities mentioned:
surface_form: Eve Cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.81305555555556
lon: -130.67555555555555
surface_form: Williams Cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.78
lon: -130.599
Radiocarbon dating of charred alpine willow twigs preserved in ejecta from Williams Cone suggests the latest eruption in the Desolation Lava Field occurred in the last 2,000 years. Geography. The Desolation Lava Field is at the northern end of the Big Raven Plateau which is bounded by Mess Creek valley in the west, Kakiddi Creek valley in the east and the Klastline River valley in the north.

Geographic entities mentioned:
surface_form: Big Raven Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.7167
lon: -130.75
surface_form: Mess Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.88296
lon: -131.2206
surface_form: Kakiddi Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.872778
lon: -130.425556
This intermontane plateau is one of the principal physiographic features of the Mount Edziza volcanic complex, a group of overlapping shield volcanoes, stratovolcanoes, lava domes and cinder cones that have formed over the last 7.5 million years. The Desolation Lava Field reaches an elevation of on the plateau, but decreases in elevation to at Buckley Lake and in the Klastline River valley.

Geographic entities mentioned:
surface_form: Mount Edziza volcanic complex
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5
lon: -130.6
Volcanic cones. The Desolation Lava Field consists of more than of blocky lava flows and wind-sculptured ash beds that were erupted from at least 10 cinder cones. Eve Cone near the middle of the lava field has an elevation of and is one of the most symmetrical and best preserved cinder cones in Canada.

Geographic entities mentioned:
surface_form: Eve Cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.81305555555556
lon: -130.67555555555555
Moraine Cone is the southernmost cinder cone and is the highest of the Desolation vents, attaining an elevation of nearly. Sidas Cone has an elevation of and is the northernmost cinder cone of the Desolation Lava Field. Sleet Cone, the southeasternmost eruptive centre of the Desolation Lava Field, has an elevation of and consists of two overlapping cones.

Geographic entities mentioned:
surface_form: Sidas Cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.8589
lon: -130.628
It has an elevation of and consists of a breached cone; the breach contains a steep-sided lava dome. Williams Cone northeast of Moraine Cone is in elevation and is the largest cone in the Desolation Lava Field, containing a basal width of. Most of the Desolation Lava Field cones are clustered near the northern base of Mount Edziza, an ice-covered stratovolcano attaining an elevation of. Geology.

Geographic entities mentioned:
surface_form: Williams Cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.78
lon: -130.599
It has an elevation of and consists of a breached cone; the breach contains a steep-sided lava dome. Williams Cone northeast of Moraine Cone is in elevation and is the largest cone in the Desolation Lava Field, containing a basal width of. Most of the Desolation Lava Field cones are clustered near the northern base of Mount Edziza, an ice-covered stratovolcano attaining an elevation of. Geology.

Geographic entities mentioned:
surface_form: Mount Edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
As a part of the Mount Edziza volcanic complex, the Desolation Lava Field lies within a broad area of volcanoes and lava flows called the Northern Cordilleran Volcanic Province, which extends from northwestern British Columbia northwards through Yukon into easternmost Alaska.

Geographic entities mentioned:
surface_form: Northern Cordilleran Volcanic Province
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7156
lon: -130.634
Filming began two months later and the two actors did not get along at all. However, they ended up falling in love and the &quot;fiancés of Europe&quot; celebrated their official engagement, organized by Romy's mother and stepfather in Morcote, Switzerland, on the shores of Lake Lugano, in front of the international press, without planning a date for a possible wedding.

Geographic entities mentioned:
surface_form: Lake Lugano
instance_of: Lake
countries: Switzerland
Italy
coordinates: lat: 46
lon: 9
DJ Hoppa. DJ Hoppa (born, April 28, 1983) is an American DJ and producer from Panorama City, Los Angeles. He was signed to rapper Hopsin's now defunct record label Funk Volume, and CEO of the San Fernando Valley independent label Broken Complex located in North Hollywood, California.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
Geography. Mossman in Far North Queensland on the Mossman River. Mossman is located on the Captain Cook Highway north of the regional city of Cairns, and east of the Mount Carbine Tableland. The Mossman River flows through the locality from west (Finlayvale / Mossman Gorge) to east (Newell / Bonnie Doon).

Geographic entities mentioned:
surface_form: Mount Carbine Tableland
instance_of: Mountain
Plateau
countries: Australia
coordinates: lat: -16.4458
lon: 145.232
Deng Deng National Park. Deng Deng National Park is a national park in Cameroon. Established in 2010, it covers an area of. Geography. Deng Deng National Park is located on the Sanaga River. Lom Pangar Reservoir lies east of the park. Deng Deng National Park is located southeast of Mbam Djerem National Park. Flora and fauna.

Geographic entities mentioned:
surface_form: Sanaga River
instance_of: Watercourse
countries: Cameroon
coordinates: lat: 3.5593388888889
lon: 9.652175
Cape Ann (Enderby Land). Cape Ann is a cape on the coast of East Antarctica, surmounted by Mount Biscoe rising to a peak of 700 metres. It was first photographed from the air in December 1929 during a Norwegian expedition led by explorer and aviator Hjalmar Riiser-Larsen.

Geographic entities mentioned:
surface_form: Mount Biscoe
instance_of: Mountain
coordinates: lat: -66.21667
lon: 51.36667
Fort Selkirk Volcanic Field. ouhs6i69qxji7yzp6jhm4h46iir" xml:space="preserve">#REDIRECT Fort Selkirk volcanic field

Geographic entities mentioned:
surface_form: fort selkirk volcanic field
instance_of: Mountain
countries: Canada
coordinates: lat: 62.93
lon: -137.38
In the 2016 census, Gormanston had a population of 17. It lies at the shoulder between Mount Lyell and Mount Owen and is south or &quot;up the hill&quot; from an equally abandoned community, the remains of the townsite of Linda which is at the northern side of the Linda Valley. History.

Geographic entities mentioned:
surface_form: Linda Valley
instance_of: Valley
countries: Australia
Nanga Parbat (disambiguation). Nanga Parbat is a mountain of the Himalayas, and the ninth-highest in the world.

Geographic entities mentioned:
surface_form: Nanga Parbat
instance_of: Mountain
countries: Pakistan
coordinates: lat: 35.239166666667
lon: 74.59
Since there was little interest from the metropolis in these lands, several Portuguese explorers began to settle spontaneously near the coast. When Portugal restored its independence from the Kingdom of Spain in 1640, there were already many &quot;estancias&quot; in the region, especially north of the Ducks' Lagoon and near the mouth of the Jacuí River.

Geographic entities mentioned:
surface_form: Ducks' Lagoon
instance_of: Lake
countries: Brazil
coordinates: lat: -31.15
lon: -51.39
Due to the growth of nearby cities such as Rio Pardo and Santo Antônio da Patrulha and in view of its privileged geographical situation, at the confluence of the two largest internal navigation routes - the Jacuí River and the Ducks' Lagoon - Porto Alegre began to become the largest commercial center in the Province.

Geographic entities mentioned:
surface_form: Ducks' Lagoon
instance_of: Lake
countries: Brazil
coordinates: lat: -31.15
lon: -51.39
Gromshin Heights. Gromshin Heights (, ‘Gromshinski Vazvisheniya’ \'grom-shin-ski v&-zvi-'she-ni-ya\) are the heights rising to 2731 m at Mount Ulmer on the east side of northern Sentinel Range in Ellsworth Mountains, Antarctica. They extend 35 km in north–south direction and 20 km in east–west direction.

Geographic entities mentioned:
surface_form: Mount Ulmer
instance_of: Mountain
coordinates: lat: -77.5833
lon: -86.15
The feature is upturned U-shaped with its interior drained by the south flowing Vicha Glacier, and its northeast side marked by the extensive Miller Bluffs. The heights are bounded by Rutford Ice Stream to the east and Newcomer Glacier to the south and west, and is connected to Mount Wyatt Earp on the northwest by Skamni Saddle, and to Mount Weems on the north by Kipra Gap.

Geographic entities mentioned:
surface_form: Mount Wyatt Earp
instance_of: Mountain
coordinates: lat: -77.56666667
lon: -86.41666667
surface_form: Mount Weems
instance_of: Mountain
coordinates: lat: -77.45
lon: -86.1667
Clear Lake (Iowa). Clear Lake is a natural spring fed body of water located in Cerro Gordo County, Iowa, near Clear Lake, Iowa. It is approximately in size. It is a popular fishing destination, with walleye, yellow bass and channel catfish. People from Des Moines and Minneapolis–Saint Paul have had homes on the shores of the lake since the 1870s.

Geographic entities mentioned:
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 43.1256
lon: -93.4247
Clear Lake (Iowa). Clear Lake is a natural spring fed body of water located in Cerro Gordo County, Iowa, near Clear Lake, Iowa. It is approximately in size. It is a popular fishing destination, with walleye, yellow bass and channel catfish. People from Des Moines and Minneapolis–Saint Paul have had homes on the shores of the lake since the 1870s.

Geographic entities mentioned:
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 43.1256
lon: -93.4247
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 43.1256
lon: -93.4247
As of 2004, the lake has seen major efforts undergone to restore its natural clarity, including filtration systems, dredging, and education of local farmers to reduce toxic pesticides from entering the lake. Clear Lake has been named the &quot;Best Iowa Lake Town&quot; by &quot;The Des Moines Register&quot; and &quot;A Top Vacation Spot&quot; by &quot;Midwest Living&quot; magazine. Boating.

Geographic entities mentioned:
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 43.1256
lon: -93.4247
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 43.1256
lon: -93.4247
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 43.1256
lon: -93.4247
Clear Lake has been named the &quot;Best Iowa Lake Town&quot; by &quot;The Des Moines Register&quot; and &quot;A Top Vacation Spot&quot; by &quot;Midwest Living&quot; magazine. Boating. Clear Lake is home to the Clear Lake Yacht Club, a sailing club in downtown Clear Lake, Iowa. Many members race and equally informally cruise the lake.

Geographic entities mentioned:
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 43.1256
lon: -93.4247
Now the island is mostly made up of trees and many other plants. Lone Tree Point, Farmers Beach, and Mcintosh Woods are also very natural, with many trees and beaches and few buildings. Notable lakeside communities include the city of Clear Lake, the smaller city of Ventura, Bayside, Dodges Point, Buzzards Bay, Tanglefoot, and Bell Harbor.

Geographic entities mentioned:
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 43.1256
lon: -93.4247
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 43.1256
lon: -93.4247
The city of Clear Lake is at the eastern side of the lake and is home to many of the lake's attractions including many restaurants, parks, city services, etc. The small town of Ventura sits on the northwestern basin of the lake. It is at the farthest part of the lake from the city of Clear Lake. Bayside is located on a peninsula south of Woodford Island.

Geographic entities mentioned:
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 43.1256
lon: -93.4247
Gufelstock. The Gufelstock is a mountain of the Glarus Alps, overlooking Schwanden in the canton of Glarus. The border with the canton of St. Gallen runs on the northern base of the mountain.

Geographic entities mentioned:
surface_form: gufelstock
instance_of: Mountain
countries: Switzerland
coordinates: lat: 47.025
lon: 9.1465555555556
Like the other rivers in the glacial valley, the Rodenbek flows in an east–west direction to the Alster, a tributary of the Elbe. As well as being home to fish that occur in the Alster, burbot, sunbleak, common dace and stickleback have also been observed in the Rodenbek.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
John A. Blatnik Bridge. The John A. Blatnik Bridge is the bridge that carries Interstate 535 (I-535) and U.S. Highway 53 (US 53) over the Saint Louis River, a tributary of Lake Superior, between Duluth, Minnesota, and Superior, Wisconsin. The bridge is long and rises up nearly above the water to accommodate the seaway shipping channel.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
Another possibility is that the name comes from the old Sami god Rana Niejta. Geography. The highest point in the municipality was the tall mountain Oksskolten. Sør-Rana encompassed an area on both sides of the middle section of the Ranfjorden around where the Sørfjorden and Elsfjorden branch off the main fjord.

Geographic entities mentioned:
surface_form: Oksskolten
instance_of: Mountain
countries: Norway
coordinates: lat: 66.012222222222
lon: 14.338611111111
Precipitable water in the atmosphere peaked near 1.8 inches just off the California coast on January 1. Normally, the Sierras get about three times more rain than the Sacramento Valley, but during this event, they got up to ten times more rain because of the wind direction and strength of the winds.

Geographic entities mentioned:
surface_form: Sacramento Valley
instance_of: Valley
countries: United States
coordinates: lat: 39
lon: -121.5
1997 Merced River flood. The January 1997 flood of the Merced River (flooded/flooded from the watershed/floodplain of the Merced River) occurred from December 31, 1996, to January 5, 1997, throughout the Yosemite Valley in Yosemite National Park, Mariposa County, California, US.

Geographic entities mentioned:
surface_form: Yosemite Valley
instance_of: Valley
countries: United States
coordinates: lat: 37.721694444444445
lon: -119.646
The black and white images in the series depict large-scale ocean waves shot by Ross while in the tumultuous surf, often up to his chest, and tethered to an assistant on land. In 2002, in order to photograph Mount Sopris in Colorado, Ross invented the R1 camera, with which he made some of the highest resolution large-scale landscape photographs in the world.

Geographic entities mentioned:
surface_form: Mount Sopris
instance_of: Mountain
countries: United States
coordinates: lat: 39.2632
lon: -107.176
Taken as a group, the &quot;Hurricanes&quot;, &quot;Horizons&quot; and &quot;Grain&quot; series compose a trilogy known as &quot;Wave Music&quot;. &quot;Mountain&quot; series. Typical of Ross’ dialectical working process, he found his next subject, far from the ocean in the Rocky Mountains of Colorado: Mount Sopris.

Geographic entities mentioned:
surface_form: Mount Sopris
instance_of: Mountain
countries: United States
coordinates: lat: 39.2632
lon: -107.176
Fino (river). The Fino is a river in eastern central Italy. Its source is near Monte Camicia in the province of Teramo in the Abruzzo region of Italy. The river flows northeast and then curves east before flowing past Bisenti. It continues flowing eastward and crosses into the province of Pescara near Elice.

Geographic entities mentioned:
surface_form: Monte Camicia
instance_of: Mountain
countries: Italy
coordinates: lat: 42.44
lon: 13.718
Bearhead Mountain (Montana). Bearhead Mountain () is located in the Lewis Range, Glacier National Park in the U.S. state of Montana. The mountain is named for &quot;kyáiyótokan&quot;, a Piegan warrior known for his war against the dreaded Assiniboine &quot;White Dog&quot;.

Geographic entities mentioned:
surface_form: bearhead mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.4242
lon: -113.356
(See also the nearby Blue Island.) At the intersection with 93rd Street is the Bronzeville Children's Museum. It is the only African-American children's museum in the U.S. South of 103rd Street, Stony Island Ave. enters the heavily industrialized region of Lake Calumet. At some points in the south suburbs, street signs for Stony Island Avenue are misspelled as Stoney Island Avenue. Expressway.

Geographic entities mentioned:
surface_form: Lake Calumet
instance_of: Lake
countries: United States
coordinates: lat: 41.68
lon: -87.59
Name. The name of the settlement was changed from &quot;Gradišče&quot; to &quot;Gradišče pri Lukovici&quot; in 1953. Church. The local church is built is dedicated to Saint Margaret (). It dates to the early 16th century. Gradišče Reservoir. South of the settlement lies the reservoir Lake Gradišče.

Geographic entities mentioned:
surface_form: Lake Gradišče
instance_of: Lake
countries: Slovenia
coordinates: lat: 46.158888888889
lon: 14.709444444444
Benjamin Creek. Benjamin Creek is a stream in Alberta, Canada. It is a tributary of Fallentimber Creek. Benjamin Creek has the name of Jonas Benjamin, a Stoney tribal leader.

Geographic entities mentioned:
surface_form: Fallentimber Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 51.7501
lon: -114.65202
Benjamin Creek. Benjamin Creek is a stream in Alberta, Canada. It is a tributary of Fallentimber Creek. Benjamin Creek has the name of Jonas Benjamin, a Stoney tribal leader.

Geographic entities mentioned:
surface_form: benjamin creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 51.53339
lon: -115.06874
From Three Rivers, Route 106 is known as the &quot;Old Post Road&quot; and crosses to the north bank of the Petitcodiac River passing the eastern terminus of Route 885. From here, the route turns northeast, traveling through Petitcodiac East, crossing Route 1 at exit 239 in River Glade and continuing to Salisbury where it briefly merges with Route 112.

Geographic entities mentioned:
surface_form: Petitcodiac River
instance_of: Watercourse
countries: Canada
coordinates: lat: 45.926944444444
lon: -65.188888888889
The road continues in a southeasterly direction where it is known as &quot;Vallee Road&quot;, passing Folly Lake as it enters Memramcook, where it turns south at the western terminus of Route 933. Here the route is known as &quot;Royal Road&quot;, passing the western terminus of Route 925 to follow the east bank of the Memramcook River passing through Upper Dorchester, Middleton, and Dorchester.

Geographic entities mentioned:
surface_form: Memramcook River
instance_of: Watercourse
countries: Canada
coordinates: lat: 45.867
lon: -64.552
Most of the headland is hilly, with peaks such as the 171 m Black Linn, by the Ben of Howth, on a side road beyond the Green Hill Quarries at the Loughereen Hills, Shielmartin Hill (163 m) overlooking Carrickbrack Road and Carrickbrack and Dun Hill. There are also craggy areas such as Muck Rock (Carrickmore), and Kilrock.

Geographic entities mentioned:
surface_form: Ben of Howth
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.373188888889
lon: -6.0700194444444
surface_form: Shielmartin Hill
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.373363888889
lon: -6.0834222222222
On clear days, the Wicklow Mountains can be seen, with Dublin city below. Slieve Donard, an 852-metre peak in Northern Ireland may also be visible - a distance of. Quite frequently, Snowdon (1,085 m) in Snowdonia National Park in Wales can also be seen - a distance of. Cultural references. Howth Head is the location where Leopold Bloom proposes to Molly in James Joyce's &quot;Ulysses&quot;.

Geographic entities mentioned:
surface_form: Slieve Donard
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.180277777778
lon: -5.9208333333333
On clear days, the Wicklow Mountains can be seen, with Dublin city below. Slieve Donard, an 852-metre peak in Northern Ireland may also be visible - a distance of. Quite frequently, Snowdon (1,085 m) in Snowdonia National Park in Wales can also be seen - a distance of. Cultural references. Howth Head is the location where Leopold Bloom proposes to Molly in James Joyce's &quot;Ulysses&quot;.

Geographic entities mentioned:
surface_form: Snowdon
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.068863888889
lon: -4.0755888888889
However, the Yenisei Kyrgyz spent much of their time in a state of rebellion. In 840 they succeeded in sacking the Uyghur capital, Ordu-Baliq in Mongolia's Orkhon Valley and driving the Uyghurs out of Mongolia entirely. On February 13, 843 at &quot;Kill the Foreigners&quot; Mountain, the Tang Chinese inflicted a devastating defeat on the Uyghur Qaghan's forces.

Geographic entities mentioned:
surface_form: Orkhon Valley
instance_of: Valley
countries: Mongolia
coordinates: lat: 47.556666666667
lon: 102.83138888889
Yellowknife Water Aerodrome. Yellowknife Water Aerodrome is an aerodrome adjacent to the &quot;old town&quot; section of Yellowknife, Northwest Territories, Canada on both Back Bay and East Bay of Great Slave Lake. It is open from the middle of June until October and may be used by ski equipped aircraft in the winter.

Geographic entities mentioned:
surface_form: Great Slave Lake
instance_of: Lake
countries: Canada
coordinates: lat: 61.666666666667
lon: -114
Location. Black horse Lake is located approximately southeast of Benton Lake National Wildlife Refuge. History. This lake was previously a large, year round lake. According to historical records, the nearby Benton Lake, was used by early European settlers in the Great Falls, Montana region, to irrigate farms. A canal or canals were dug to drain Benton Lake for irrigation.

Geographic entities mentioned:
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 43.9344286
lon: -96.9790408
surface_form: round lake
instance_of: Body of water
countries: United States
coordinates: lat: 44.0648
lon: -75.1033
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 46.1508
lon: -86.7447
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 44.070277777778
lon: -74.584722222222
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 42.934604
lon: -73.7823057
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 27.9631
lon: -81.674
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 45.036388888889
lon: -97.773055555556
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 43.531388888889
lon: -75.180277777778
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 44.8685
lon: -93.4925
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 48.161666666667
lon: -116.63805555556
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 45.6020431
lon: -122.4032555
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 41.837095
lon: -86.418541
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 44.964444444444
lon: -96.827222222222
Black Horse Lake. Black Horse Lake is a seasonal lake just north of present-day Great Falls, Montana. The lake is usually dry, except during the spring and early summer. Location. Black horse Lake is located approximately southeast of Benton Lake National Wildlife Refuge. History. This lake was previously a large, year round lake.

Geographic entities mentioned:
surface_form: benton lake
instance_of: Lake
countries: United States
coordinates: lat: 47.68611111111111
lon: -111.35222222222221
surface_form: black horse lake
instance_of: Lake
countries: United States
coordinates: lat: 47.6058
lon: -111.221
History. This lake was previously a large, year round lake. According to historical records, the nearby Benton Lake, was used by early European settlers in the Great Falls, Montana region, to irrigate farms. A canal or canals were dug to drain Benton Lake for irrigation. The one remaining canal leads from northwest to southeast, directly to Black Horse Lake.

Geographic entities mentioned:
surface_form: benton lake
instance_of: Lake
countries: United States
coordinates: lat: 47.68611111111111
lon: -111.35222222222221
The one remaining canal leads from northwest to southeast, directly to Black Horse Lake. The canal abruptly stops about a third of a mile from where Black Horse Lake was situated. Black Horse lake is above sea level while nearby Benton Lake is above sea level. In 2008 the United States Department of Energy obliged Montana Alberta Tie Ltd to route power-lines away from the lake. Ecology.

Geographic entities mentioned:
surface_form: benton lake
instance_of: Lake
countries: United States
coordinates: lat: 47.68611111111111
lon: -111.35222222222221
surface_form: black horse lake
instance_of: Lake
countries: United States
coordinates: lat: 47.6058
lon: -111.221
Black Horse Lake. Black Horse Lake is a seasonal lake just north of present-day Great Falls, Montana. The lake is usually dry, except during the spring and early summer. Location. Black horse Lake is located approximately southeast of Benton Lake National Wildlife Refuge. History. This lake was previously a large, year round lake.

Geographic entities mentioned:
surface_form: black horse lake
instance_of: Lake
countries: United States
coordinates: lat: 47.6058
lon: -111.221
According to historical records, the nearby Benton Lake, was used by early European settlers in the Great Falls, Montana region, to irrigate farms. A canal or canals were dug to drain Benton Lake for irrigation. The one remaining canal leads from northwest to southeast, directly to Black Horse Lake. The canal abruptly stops about a third of a mile from where Black Horse Lake was situated.

Geographic entities mentioned:
surface_form: black horse lake
instance_of: Lake
countries: United States
coordinates: lat: 47.6058
lon: -111.221
A canal or canals were dug to drain Benton Lake for irrigation. The one remaining canal leads from northwest to southeast, directly to Black Horse Lake. The canal abruptly stops about a third of a mile from where Black Horse Lake was situated. Black Horse lake is above sea level while nearby Benton Lake is above sea level.

Geographic entities mentioned:
surface_form: black horse lake
instance_of: Lake
countries: United States
coordinates: lat: 47.6058
lon: -111.221
Ecology. The lake is an alkali wetlands and a habitat to waterfowl, gulls and shorebirds. It floods seasonally. Size. The present size of Black Horse Lake varies due to varying precipitation and other factors. In dry years, the lake never fills up at all. The lakes maximum extent is 1.5 miles from north to south, and 1.25 miles from east to west covering an area of.

Geographic entities mentioned:
surface_form: black horse lake
instance_of: Lake
countries: United States
coordinates: lat: 47.6058
lon: -111.221
Little River Canyon National Preserve. Little River Canyon National Preserve is a United States National Preserve located on top of Lookout Mountain near Fort Payne, Alabama, and DeSoto State Park. Created by an Act of Congress in 1992, the preserve protects what is sometimes said to be the nation's longest mountaintop river, the Little River.

Geographic entities mentioned:
surface_form: Lookout Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 34.863713888889
lon: -85.392452777778
Created by an Act of Congress in 1992, the preserve protects what is sometimes said to be the nation's longest mountaintop river, the Little River. The canyon was historically called &quot;May's Gulf&quot;, &quot;gulf&quot; being a common term throughout the Cumberland Plateau for this sort of feature.

Geographic entities mentioned:
surface_form: Cumberland Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 36
lon: -85
The river. The Little River flows for almost its entire length along the middle of Lookout Mountain in northeast Alabama. Over eons of geologic time, Little River has carved out one of the Southeast's deepest canyons as it winds its way from headwaters in Georgia before exiting the mountain and emptying into the Coosa River (Weiss Lake impoundment) near Leesburg, Alabama.

Geographic entities mentioned:
surface_form: Coosa River
instance_of: Watercourse
countries: United States
coordinates: lat: 32.4862464
lon: -86.2777475
Throughout its history, Lohnstorf has been part of the large parish of Thurnen which is centered in Kirchenthurnen. The Gürbe river correction projects of 1855-1911 helped drain the marshy valley floor and opened up farmland. Today, agriculture is the major industry in the municipality, though about two-thirds of the work force commute to jobs in surrounding towns and cities.

Geographic entities mentioned:
surface_form: Gürbe river
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.836111111111
lon: 7.5063888888889
All the water in the municipality is flowing water. The municipality and village or Lohnstorf are located in the Gürbetal (Gürbe valley) near Längenberg mountain. On 31 December 2009 Amtsbezirk Seftigen, the municipality's former district, was dissolved. On the following day, 1 January 2010, it joined the newly created Verwaltungskreis Bern-Mittelland. Coat of arms.

Geographic entities mentioned:
surface_form: Gürbetal
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.836111111111
lon: 7.5063888888889
BB&T (now Truist Financial) acquired UCB in 1997. History. In 1926, business people in Whiteville raised $10,000 and started Waccamaw Bank and Trust, named for an area Lake Waccamaw and the Waccamaw River. American Bank & Trust of Monroe, North Carolina began May 5, 1930 in the Monroe Hotel after the bank failure of Bank of Union during the Great Depression.

Geographic entities mentioned:
surface_form: Lake Waccamaw
instance_of: Lake
countries: United States
coordinates: lat: 34.2867009
lon: -78.509745
Vatndalsvatnet. Vatndalsvatnet or Vatnedalsvatnet is a lake in the municipality of Bykle in Agder county, Norway. The lake lies about west of the village of Berdalen and the river Otra. The nearby lakes Ormsavatnet and Store Urevatn flow into the lake through dams and canals. The lake Vatndalsvatnet also has a dam on it and the water flows out of the lake from the dam into the Otra river.

Geographic entities mentioned:
surface_form: Ormsavatnet
instance_of: Lake
countries: Norway
coordinates: lat: 59.521388888889
lon: 7.1155555555556
surface_form: Store Urevatn
instance_of: Lake
countries: Norway
coordinates: lat: 59.456111111111
lon: 7.1058333333333
The nearby lakes Ormsavatnet and Store Urevatn flow into the lake through dams and canals. The lake Vatndalsvatnet also has a dam on it and the water flows out of the lake from the dam into the Otra river. It is located in the central part of Bykle, about halfway between the villages of Hovden and Bykle. The mountains Snjoheinuten and Kvervetjønnuten both lie on the south side of the lake.

Geographic entities mentioned:
surface_form: Snjoheinuten
instance_of: Mountain
countries: Norway
coordinates: lat: 59.4225
lon: 7.255
surface_form: Kvervetjønnuten
instance_of: Mountain
countries: Norway
coordinates: lat: 59.4339
lon: 7.3084
Mogollon Baldy Lookout Cabin. The Mogollon Baldy Lookout Cabin, in Gila National Forest on Mogollon Baldy peak, in New Mexico, was built in 1923. It was listed on the National Register of Historic Places in 1988. It is a log cabin close to the lookout tower near the peak. The listing does not include the lookout tower itself. It is located on Mogollon Baldy, a peak in the Mogollons.

Geographic entities mentioned:
surface_form: Mogollon Baldy
instance_of: Mountain
countries: United States
coordinates: lat: 33.271388888889
lon: -108.59472222222
It was listed on the National Register of Historic Places in 1988. It is a log cabin close to the lookout tower near the peak. The listing does not include the lookout tower itself. It is located on Mogollon Baldy, a peak in the Mogollons. The highest peak in the Mogollons, Whitewater Baldy, is to the northwest.

Geographic entities mentioned:
surface_form: Mogollon Baldy
instance_of: Mountain
countries: United States
coordinates: lat: 33.271388888889
lon: -108.59472222222
It was listed on the National Register of Historic Places in 1988. It is a log cabin close to the lookout tower near the peak. The listing does not include the lookout tower itself. It is located on Mogollon Baldy, a peak in the Mogollons. The highest peak in the Mogollons, Whitewater Baldy, is to the northwest.

Geographic entities mentioned:
surface_form: Whitewater Baldy
instance_of: Mountain
countries: United States
coordinates: lat: 33.323611111111
lon: -108.64111111111
Wadi al-Taym. Wadi al-Taym (), also transliterated as Wadi el-Taym, is a wadi (dry river) that forms a large fertile valley in Lebanon, in the districts of Rachaya and Hasbaya on the western slopes of Mount Hermon. It adjoins the Beqaa Valley running north to south towards the Jordan Valley where it meets the northwest corner of Lake Huleh.

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
Wadi al-Taym. Wadi al-Taym (), also transliterated as Wadi el-Taym, is a wadi (dry river) that forms a large fertile valley in Lebanon, in the districts of Rachaya and Hasbaya on the western slopes of Mount Hermon. It adjoins the Beqaa Valley running north to south towards the Jordan Valley where it meets the northwest corner of Lake Huleh.

Geographic entities mentioned:
surface_form: Beqaa Valley
instance_of: Valley
countries: Lebanon
coordinates: lat: 34.008888888889
lon: 36.145277777778
For much of the early 12th century, the Wadi al-Taym and the southern Chouf were the territory of the Jandal, a Druze clan. The leader of the clan, Dahhak ibn Jandal allied with the Crusaders of the Kingdom of Jerusalem and engaged in a feud with the Assassins who ruled the Banias fortress in the western foothills of Mount Hermon just south of Wadi al-Taym.

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
In 1149, Dahhak was himself murdered by Assassins, revenge for the slaying of the &quot;da'i&quot;. The Wadi al-Taym was taken over by the Shihabs, a Sunni Muslim clan in the army of the Ayyubid sultan Saladin, in 1173. The Shihab formed an alliance with the Druze Ma'n family of southern Mount Lebanon.

Geographic entities mentioned:
surface_form: mount lebanon
instance_of: Mountain
countries: Lebanon
coordinates: lat: 34.3
lon: 36.116666666667
The Shihab formed an alliance with the Druze Ma'n family of southern Mount Lebanon. Unlike other immigrants to the Wadi al-Taym, the Shihabs did not embrace the Druze faith, which was the dominant religion of the areas between the Gharb district of southern Mount Lebanon southward to the Wadi al-Taym.

Geographic entities mentioned:
surface_form: mount lebanon
instance_of: Mountain
countries: Lebanon
coordinates: lat: 34.3
lon: 36.116666666667
surface_form: wadi al-taym
instance_of: Valley
countries: Lebanon
coordinates: lat: 33.4333
lon: 35.7
Wadi al-Taym. Wadi al-Taym (), also transliterated as Wadi el-Taym, is a wadi (dry river) that forms a large fertile valley in Lebanon, in the districts of Rachaya and Hasbaya on the western slopes of Mount Hermon. It adjoins the Beqaa Valley running north to south towards the Jordan Valley where it meets the northwest corner of Lake Huleh.

Geographic entities mentioned:
surface_form: wadi al-taym
instance_of: Valley
countries: Lebanon
coordinates: lat: 33.4333
lon: 35.7
It adjoins the Beqaa Valley running north to south towards the Jordan Valley where it meets the northwest corner of Lake Huleh. Watered by the Hasbani river, the low hills of Wadi al-Taym are covered with rows of silver-green olive trees with the population in the area being predominantly Druze and Sunni, with a high number of Christians, mostly Greek Orthodox.

Geographic entities mentioned:
surface_form: wadi al-taym
instance_of: Valley
countries: Lebanon
coordinates: lat: 33.4333
lon: 35.7
Watered by the Hasbani river, the low hills of Wadi al-Taym are covered with rows of silver-green olive trees with the population in the area being predominantly Druze and Sunni, with a high number of Christians, mostly Greek Orthodox. Wadi al-Taym is generally considered the &quot;birthplace of the Druze faith&quot;. History.

Geographic entities mentioned:
surface_form: wadi al-taym
instance_of: Valley
countries: Lebanon
coordinates: lat: 33.4333
lon: 35.7
History. Wadi al-Taym is named after the Arab tribe of Taym Allat (later Taym-Allah) ibn Tha'laba. The Taym-Allat entered the Euphrates Valley and adopted Christianity in the pre-Islamic period before ultimately embracing Islam after the 7th-century Muslim conquests. A small proportion of the tribe took up abode in the Wadi al-Taym at some point during the first centuries of Muslim rule.

Geographic entities mentioned:
surface_form: wadi al-taym
instance_of: Valley
countries: Lebanon
coordinates: lat: 33.4333
lon: 35.7
surface_form: wadi al-taym
instance_of: Valley
countries: Lebanon
coordinates: lat: 33.4333
lon: 35.7
According to the historian Nejla Abu-Izzedin, &quot;ethnically&quot;, the &quot;Wadi al-Taym has been authoritatively stated to be one of the most Arab regions of [geographical] Syria&quot;. The area was one of the two most important centers of Druze missionary activity in the 11th century.

Geographic entities mentioned:
surface_form: wadi al-taym
instance_of: Valley
countries: Lebanon
coordinates: lat: 33.4333
lon: 35.7
The area was one of the two most important centers of Druze missionary activity in the 11th century. For much of the early 12th century, the Wadi al-Taym and the southern Chouf were the territory of the Jandal, a Druze clan.

Geographic entities mentioned:
surface_form: wadi al-taym
instance_of: Valley
countries: Lebanon
coordinates: lat: 33.4333
lon: 35.7
Unlike other immigrants to the Wadi al-Taym, the Shihabs did not embrace the Druze faith, which was the dominant religion of the areas between the Gharb district of southern Mount Lebanon southward to the Wadi al-Taym. In 1287, the Shihab emir Sa'ad ibn Qurqmaz, now allied with the Mamluk successors of the Ayyubids, confronted a Mongol incursion into the Wadi al-Taym.

Geographic entities mentioned:
surface_form: wadi al-taym
instance_of: Valley
countries: Lebanon
coordinates: lat: 33.4333
lon: 35.7
Geography. Shelley Lake is located in the Veradale area of the city of Spokane Valley approximately one-half mile south of Sprague Avenue, the main east–west surface street in the Valley. The lake is located on the relatively flat floor of the Spokane Valley, just below hills which rise to the south into the uplands which comprise most of the lake's drainage basin.

Geographic entities mentioned:
surface_form: Spokane Valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
Shelley Lake. Shelley Lake is a small lake located entirely in the city of Spokane Valley, in the U.S. state of Washington. The lake is surrounded on three sides by the 248 lot gated community of Shelley Lake Estates. The lake is kept full by Saltese Creek, which is supplied by drainage canals from the Saltese Flats. Although an open lake, there are no above-ground outflows. Geography.

Geographic entities mentioned:
surface_form: shelley lake
instance_of: Lake
countries: United States
coordinates: lat: 47.65138888888889
lon: -117.185
Shelley Lake. Shelley Lake is a small lake located entirely in the city of Spokane Valley, in the U.S. state of Washington. The lake is surrounded on three sides by the 248 lot gated community of Shelley Lake Estates. The lake is kept full by Saltese Creek, which is supplied by drainage canals from the Saltese Flats. Although an open lake, there are no above-ground outflows. Geography.

Geographic entities mentioned:
surface_form: shelley lake
instance_of: Lake
countries: United States
coordinates: lat: 47.65138888888889
lon: -117.185
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222