Sarmila/GeoWiki-Features huggingface dataset:
The valley covers an area of about in southern Ventura County, bordering the San Fernando Valley in Los Angeles County. The Santa Clara River Valley occupies the northwestern corner of the valley. Mountainous terrain of South Mountain and Oak Ridge characterizes the northern and central area. Elevation within the quadrangle ranges from about along the arroyo bottoms to over.

Geographic entities mentioned:
surface_form: oak ridge
instance_of: Landform
countries: United States
coordinates: lat: 37.46
lon: -121.722
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.182222222222
lon: -74.477777777778
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.949166666667
lon: -74.293333333333
surface_form: south mountain
instance_of: Landform
countries: United States
coordinates: lat: 40.33
lon: -76.2
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.5544
lon: -72.8236
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.40111111
lon: -109.26111111
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.189166666667
lon: -74.051666666667
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.361944444444
lon: -74.285277777778
Mountainous terrain of South Mountain and Oak Ridge characterizes the northern and central area. Elevation within the quadrangle ranges from about along the arroyo bottoms to over. Steep, highly dissected slopes form much of the boundary of the area. In the southeast, Little Simi Valley, drained by Arroyo Simi/Arroyo Las Posas, separates the southern flank of Oak Ridge from the Las Posas Hills.

Geographic entities mentioned:
surface_form: oak ridge
instance_of: Landform
countries: United States
coordinates: lat: 37.46
lon: -121.722
surface_form: simi valley
instance_of: Valley
countries: United States
coordinates: lat: 34.27833333
lon: -118.71083333
This relatively low-lying area is also referred to as the Las Posas Valley. Numerous north-south-trending drainages cut South Mountain and Oak Ridge creating steep narrow canyons on north-facing slopes and wide flat-bottomed canyons with incised streams on south-facing slopes. A network of residential streets and ranch and oilfield roads that traverse the area from U.S.

Geographic entities mentioned:
surface_form: oak ridge
instance_of: Landform
countries: United States
coordinates: lat: 37.46
lon: -121.722
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.182222222222
lon: -74.477777777778
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.949166666667
lon: -74.293333333333
surface_form: south mountain
instance_of: Landform
countries: United States
coordinates: lat: 40.33
lon: -76.2
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.5544
lon: -72.8236
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.40111111
lon: -109.26111111
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.189166666667
lon: -74.051666666667
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.361944444444
lon: -74.285277777778
Deep-marine strata of the upper Miocene Modelo Formation cover the Vaqueros Formation and Topanga Group along the crests and southern flanks of South Mountain and Oak Ridge. They also occur as isolated outcrops in the Las Posas Hills. Locally, Modelo Formation consists of interbedded diatomaceous shale, claystone, mudstone, and siltstone with minor sandstone, limestone, chert, and tuff beds.

Geographic entities mentioned:
surface_form: oak ridge
instance_of: Landform
countries: United States
coordinates: lat: 37.46
lon: -121.722
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.182222222222
lon: -74.477777777778
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.949166666667
lon: -74.293333333333
surface_form: south mountain
instance_of: Landform
countries: United States
coordinates: lat: 40.33
lon: -76.2
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.5544
lon: -72.8236
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.40111111
lon: -109.26111111
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.189166666667
lon: -74.051666666667
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.361944444444
lon: -74.285277777778
Locally, Modelo Formation consists of interbedded diatomaceous shale, claystone, mudstone, and siltstone with minor sandstone, limestone, chert, and tuff beds. The most widely exposed rock units in the area are the Plio-Pleistocene marine and non-marine Pico and Saugus Formations that crop out on the southern flank of South Mountain-Oak Ridge.

Geographic entities mentioned:
surface_form: oak ridge
instance_of: Landform
countries: United States
coordinates: lat: 37.46
lon: -121.722
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.182222222222
lon: -74.477777777778
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.949166666667
lon: -74.293333333333
surface_form: south mountain
instance_of: Landform
countries: United States
coordinates: lat: 40.33
lon: -76.2
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.5544
lon: -72.8236
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.40111111
lon: -109.26111111
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.189166666667
lon: -74.051666666667
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.361944444444
lon: -74.285277777778
Simi Valley (valley). Simi Valley (Chumash: &quot;Shimiyi&quot;) is a synclinal valley in Southern California in the United States. It is an enclosed or hidden valley surrounded by mountains and hills.

Geographic entities mentioned:
surface_form: hidden valley
instance_of: Valley
countries: United States
coordinates: lat: 34.1390809
lon: -118.8768813
surface_form: hidden valley
instance_of: Landform
countries: United States
coordinates: lat: 37.2431
lon: -80.0403
Simi Valley (valley). Simi Valley (Chumash: &quot;Shimiyi&quot;) is a synclinal valley in Southern California in the United States. It is an enclosed or hidden valley surrounded by mountains and hills.

Geographic entities mentioned:
surface_form: simi valley (valley)
instance_of: Valley
countries: United States
coordinates: lat: 34.27833333
lon: -118.71083333
Simi Valley (valley). Simi Valley (Chumash: &quot;Shimiyi&quot;) is a synclinal valley in Southern California in the United States. It is an enclosed or hidden valley surrounded by mountains and hills.

Geographic entities mentioned:
surface_form: simi valley
instance_of: Valley
countries: United States
coordinates: lat: 34.27833333
lon: -118.71083333
Highway 101 and state highways 118, 23, and 126 provides access to the area. Current land use includes citrus and avocado orchards, oil well drilling and production, sand and gravel quarries, decorative-rock quarries, cattle grazing, suburban residential development, and golf courses. The oldest geologic unit mapped in the Simi Valley quadrangle is the upper Cretaceous Chatsworth Formation.

Geographic entities mentioned:
surface_form: simi valley
instance_of: Valley
countries: United States
coordinates: lat: 34.27833333
lon: -118.71083333
However, substantial late Quaternary offset is suggested by the presence of more than 150 m of Pleistocene and younger alluvium that fills the east-west trending, down-dropped bedrock trough beneath western Simi Valley. In addition, trenching within faulted colluvial deposits in Tierra Rejada Valley has revealed evidence of multiple shears within Holocene deposits.

Geographic entities mentioned:
surface_form: simi valley
instance_of: Valley
countries: United States
coordinates: lat: 34.27833333
lon: -118.71083333
Seismic and well data from the San Fernando Valley document evolution of that region from mid-Miocene rifting to north-south contraction. Formations in the western San Fernando Valley subsurface (Cretaceous to Paleogene strata, and Miocene Topanga and Modelo Formations) trace southward to outcrops in the Santa Monica Mountains that constrain faulting along the valley's south basin edge.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: san fernando valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
Cretaceous strata in the Simi Uplift to the west are over 2 km higher than equivalent strata beneath the western San Fernando Valley across a boundary marked by the Chatsworth Reservoir fault, and Neogene thinning and off-lap. The Simi fault, located at the eastern end of the Simi-Santa Rosa fault system, bounds the northern margins of the Simi and Tierra Rejada Valleys.

Geographic entities mentioned:
surface_form: san fernando valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
The northern end of larger lake Karasor lies to the east. Smaller lake Zhyngyldy, with the Ekibastuz GRES-1 Power Station by its northern shore, lies to the south of the southern lakeshore. Lake Tuzdysor lies to the northeast and Shureksor in the same direction. Shandaksor usually freezes in November and thaws in April.

Geographic entities mentioned:
surface_form: Shureksor
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 52.24261
lon: 75.79811
Fagatogo, American Samoa. Fagatogo () is the downtown area of Pago Pago (the territorial capital of American Samoa). Located in the low grounds at the foot of Matafao Peak, it was the location of the first American settlement on Tutuila Island. It includes the sub-village of Malaloa. Today, Fagatogo is the government, commercial, financial, and shipping center of Tutuila.

Geographic entities mentioned:
surface_form: Matafao Peak
instance_of: Mountain
countries: United States
coordinates: lat: -14.29972
lon: -170.7025
Residents from all over the island travel to it by bus. Several landmarks are visible from the market: Mount ʻAlava, the canneries in Atu'u, Rainmaker Mountain (Mount Pioa), and Pago Pago Harbor. Immediately next to the Fagatogo Market is the Fagatogo Square Shopping Center, a retail- and commercial center containing a number of large shops and restaurants.

Geographic entities mentioned:
surface_form: Mount ʻAlava
instance_of: Mountain
countries: United States
coordinates: lat: -14.2656
lon: -170.6881
surface_form: Rainmaker Mountain
instance_of: Mountain
countries: United States
coordinates: lat: -14.276388888889
lon: -170.65277777778
Souvenirs are often sold at the market when cruise ships are visiting town. Locals also sell handmade crafts at the dock and on the main street. Mount ʻAlava, the canneries in Atu'u, Rainmaker Mountain (Mount Pioa), and Pago Pago Harbor are all visible from the market. The main bus station is located immediately behind the market.

Geographic entities mentioned:
surface_form: Rainmaker Mountain
instance_of: Mountain
countries: United States
coordinates: lat: -14.276388888889
lon: -170.65277777778
Description. The shell is small, turbinate and thin. The nacre shines with a peculiarly coppery luster. The apex is white. The periphery is painted with purple-brown flammules and the spirals are more or less articulated with the same color. The columella is white. Distribution. This species occurs in the Pacific Ocean from Point Conception to San Diego, California.

Geographic entities mentioned:
surface_form: Point Conception
instance_of: Landform
countries: United States
coordinates: lat: 34.448113
lon: -120.471439
Historically, the lowland European bison's range encompassed most of the lowlands of northern Europe, extending from the Massif Central to the Volga River and the Caucasus. It may have once lived in the Asiatic part of what is now the Russian Federation, reaching to Lake Baikal and Altai Mountains in east.

Geographic entities mentioned:
surface_form: Lake Baikal
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.30277778
lon: 108.00472222
Its population in Gaul was extinct in the 8th century AD. The species survived in the Ardennes and the Vosges Mountains until the 15th century. In the Early Middle Ages, the wisent apparently still occurred in the forest steppes east of the Urals, in the Altai Mountains, and seems to have reached Lake Baikal in the east. The northern boundary in the Holocene was probably around 60°N in Finland.

Geographic entities mentioned:
surface_form: Lake Baikal
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.30277778
lon: 108.00472222
It continues to wind its way northeast, then east through farmland for several miles, where it passes through the community of Ogden, before coming to an end at another intersection with SR 30, just across Walden Ridge from Dayton. The entire route of SR 443 is a two-lane highway and lies entirely atop the Cumberland Plateau.

Geographic entities mentioned:
surface_form: Cumberland Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 36
lon: -85
Parish church of Urtijëi. The Parish Church of Urtijëi located in the town of Urtijëi in Val Gardena in South Tyrol, Italy is dedicated to the Epiphany and to Saint Ulrich. It was built in the years 1792&ndash;1796 in the Neoclassical style with some Baroque elements by the tyrolean master Joseph Abenthung and the interior domes painted by the Tyrolean brothers Franz Xaver and Josef Kirchebner.

Geographic entities mentioned:
surface_form: Val Gardena
instance_of: Valley
countries: Italy
coordinates: lat: 46.56
lon: 11.704722
Canaan Street Lake. Canaan Street Lake is a water body located in Grafton County in western New Hampshire, United States, in the town of Canaan. It is part of the Mascoma River watershed, a tributary of the Connecticut River. A peninsula on the north side of the lake is occupied by the Cardigan Mountain School. The west side of the lake is bordered by the Canaan Street Historic District.

Geographic entities mentioned:
surface_form: canaan street lake
instance_of: Lake
countries: United States
coordinates: lat: 43.666666666667
lon: -72.035833333333
The town of Jasper is situated to the north-northeast. Circus Valley lies at the south side of the mountain, and the northeast aspect towers above the head of the valley of Whistlers Creek. Its nearest higher peak is Mount Estella, to the southwest, and Terminal Mountain lies to the east.

Geographic entities mentioned:
surface_form: Terminal Mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 52.778333333333336
lon: -118.16027777777778
surface_form: mount estella
instance_of: Mountain
countries: Canada
coordinates: lat: 52.76694444444445
lon: -118.21138888888889
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
This mountain's toponym was officially adopted in 1951 by the Geographical Names Board of Canada. Climate. Based on the Köppen climate classification, Manx Peak is located in a subarctic climate zone with cold, snowy winters, and mild summers. Winter temperatures can drop below with wind chill factors below. Precipitation runoff from Manx Peak drains into tributaries of the Athabasca River.

Geographic entities mentioned:
surface_form: athabasca
instance_of: Lake
countries: Canada
coordinates: lat: 59.266666666667
lon: -109.45
surface_form: athabasca
instance_of: Mountain
countries: Canada
coordinates: lat: 52.18055555555556
lon: -117.20166666666667
surface_form: manx peak
instance_of: Mountain
countries: Canada
coordinates: lat: 52.7775
lon: -118.19166666666666
Manx Peak. Manx Peak is a mountain summit located in Jasper National Park, in the Trident Range of the Canadian Rockies of Alberta, Canada. The town of Jasper is situated to the north-northeast. Circus Valley lies at the south side of the mountain, and the northeast aspect towers above the head of the valley of Whistlers Creek.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: manx peak
instance_of: Mountain
countries: Canada
coordinates: lat: 52.7775
lon: -118.19166666666666
The town of Jasper is situated to the north-northeast. Circus Valley lies at the south side of the mountain, and the northeast aspect towers above the head of the valley of Whistlers Creek. Its nearest higher peak is Mount Estella, to the southwest, and Terminal Mountain lies to the east.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
History. The peak was named in 1916 by Morrison P. Bridgland because the shape of the contours of the mountain resemble the triskelion in the flag of the Isle of Man, the home of the Manx people. Bridgland (1878–1948), was a Dominion Land Surveyor who named many peaks in Jasper Park and the Canadian Rockies. The first ascent of Manx Peak was made in 1919 by R.T. Chamberlin and B. Herzberg.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
The first ascent of Manx Peak was made in 1919 by R.T. Chamberlin and B. Herzberg. This mountain's toponym was officially adopted in 1951 by the Geographical Names Board of Canada. Climate. Based on the Köppen climate classification, Manx Peak is located in a subarctic climate zone with cold, snowy winters, and mild summers. Winter temperatures can drop below with wind chill factors below.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Manx Peak. Manx Peak is a mountain summit located in Jasper National Park, in the Trident Range of the Canadian Rockies of Alberta, Canada. The town of Jasper is situated to the north-northeast. Circus Valley lies at the south side of the mountain, and the northeast aspect towers above the head of the valley of Whistlers Creek.

Geographic entities mentioned:
surface_form: manx peak
instance_of: Mountain
countries: Canada
coordinates: lat: 52.7775
lon: -118.19166666666666
History. The peak was named in 1916 by Morrison P. Bridgland because the shape of the contours of the mountain resemble the triskelion in the flag of the Isle of Man, the home of the Manx people. Bridgland (1878–1948), was a Dominion Land Surveyor who named many peaks in Jasper Park and the Canadian Rockies. The first ascent of Manx Peak was made in 1919 by R.T. Chamberlin and B. Herzberg.

Geographic entities mentioned:
surface_form: manx peak
instance_of: Mountain
countries: Canada
coordinates: lat: 52.7775
lon: -118.19166666666666
This mountain's toponym was officially adopted in 1951 by the Geographical Names Board of Canada. Climate. Based on the Köppen climate classification, Manx Peak is located in a subarctic climate zone with cold, snowy winters, and mild summers. Winter temperatures can drop below with wind chill factors below. Precipitation runoff from Manx Peak drains into tributaries of the Athabasca River.

Geographic entities mentioned:
surface_form: manx peak
instance_of: Mountain
countries: Canada
coordinates: lat: 52.7775
lon: -118.19166666666666
She also took a paid position with the local Farm Loan Association, dispensing small loans to local farmers. Wilder's column in the &quot;Ruralist&quot;, &quot;As a Farm Woman Thinks,&quot; introduced her to a loyal audience of rural Ozarkians, who enjoyed her regular columns.

Geographic entities mentioned:
surface_form: Ozarkians
instance_of: Plateau
countries: United States
coordinates: lat: 37.1822
lon: -92.5159
__NOTOC__
Asiru Qucha (Aymara &quot;asiru&quot; snake, Quechua &quot;qucha&quot; lake, Hispanicized spellings &quot;Acero Cocha, Acero Khocha, Acero Q'ocha&quot;) is a Bolivian lake located in the Vacas Municipality, Arani Province, Cochabamba Department. The main tributaries of Asiru Qucha are Asiru Qucha River, Chillawi P'ujru, Inka Mayu with Q'asa Mayu, Juq'ullu Mayu, and Pisqu Mayu.

Geographic entities mentioned:
surface_form: inka
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.4822
lon: -67.8303
surface_form: asiru qucha
instance_of: Lake
countries: Bolivia
coordinates: lat: -17.60416667
lon: -65.60138889
Asiru Qucha. __NOTOC__
Asiru Qucha (Aymara &quot;asiru&quot; snake, Quechua &quot;qucha&quot; lake, Hispanicized spellings &quot;Acero Cocha, Acero Khocha, Acero Q'ocha&quot;) is a Bolivian lake located in the Vacas Municipality, Arani Province, Cochabamba Department.

Geographic entities mentioned:
surface_form: asiru qucha
instance_of: Lake
countries: Bolivia
coordinates: lat: -17.60416667
lon: -65.60138889
Asiru Qucha. __NOTOC__
Asiru Qucha (Aymara &quot;asiru&quot; snake, Quechua &quot;qucha&quot; lake, Hispanicized spellings &quot;Acero Cocha, Acero Khocha, Acero Q'ocha&quot;) is a Bolivian lake located in the Vacas Municipality, Arani Province, Cochabamba Department.

Geographic entities mentioned:
surface_form: asiru qucha
instance_of: Lake
countries: Bolivia
coordinates: lat: -17.60416667
lon: -65.60138889
surface_form: asiru qucha
instance_of: Lake
countries: Bolivia
coordinates: lat: -17.60416667
lon: -65.60138889
(WSI), the operator of Whitefish Mountain Resort, in Whitefish, Montana. Foley's takeover of WSI occurred through a series of two reverse stock splits that took WSI from a publicly traded company, with many shareholders living in the local Flathead Valley, to a private S corp. Foley was able to purchase 27% of the outstanding WSI shares in the early 2000s from Richard A.

Geographic entities mentioned:
surface_form: Flathead Valley
instance_of: Valley
countries: United States
coordinates: lat: 48
lon: -114
Smaller populations are scattered around the South Island, including: Cook Strait, Kaikōura, Catlins (e.g., Porpoise Bay, Curio Bay), and Otago coasts (e.g.Karitane, Oamaru, Moeraki, Otago Harbour, and Blueskin Bay). Māui dolphin are typically found on the west coast of the North Island between Maunganui Bluff and Whanganui.

Geographic entities mentioned:
surface_form: Maunganui Bluff
instance_of: Mountain
countries: New Zealand
coordinates: lat: -35.75801
lon: 173.562514
Xiangkhouang. Xiangkhouang (Lao: ຊຽງຂວາງ, meaning 'Horizontal City') is a province of Laos on the Xiangkhoang Plateau, in the nation's northeast. The province has the distinction of being the most heavily bombed place on Earth. Historically, the province was formerly the independent principality of Muang Phuan. Its later capital is Phonsavan.

Geographic entities mentioned:
surface_form: Xiangkhoang Plateau
instance_of: Plateau
countries: Laos
coordinates: lat: 19.4
lon: 103.033
The plateau is characterized by rolling hills and grassland whose elevation averages. The country's highest peak, Phou Bia (), rises at the south side of the plateau. Nam Et-Phou Louey is a National Biodiversity Conservation Area (NBCA) in the province, covering an area of 5,959 km2, and overlaps into Houaphanh and Luang Prabang provinces.

Geographic entities mentioned:
surface_form: Phou Bia
instance_of: Mountain
countries: Laos
coordinates: lat: 18.983333333333
lon: 103.13333333333
They established an overland trade in metals and forest products with India and China; the Xieng Khouang Plateau was the center of trade for an area of upland Southeast Asia, extending as far as Da Nang in Vietnam, Samrong Sen in Cambodia, the Khorat Plateau in northeast Thailand, and the North Cachar Hills of northeastern India.

Geographic entities mentioned:
surface_form: Khorat Plateau
instance_of: Plateau
countries: Thailand
coordinates: lat: 15.666666666667
lon: 103.16666666667
Apart from floodplains, the largest expanse of level land in the country is on the province's Xiangkhoang Plateau. This area is characterized by rolling hills and grassland whose elevation averages. The country's highest peak, Phou Bia (), rises at the southern side of the plateau, while the Plain of Jars is at the plateau's centre. The province is 400 km northeast of Vientiane.

Geographic entities mentioned:
surface_form: Phou Bia
instance_of: Mountain
countries: Laos
coordinates: lat: 18.983333333333
lon: 103.13333333333
The province is 400 km northeast of Vientiane. Phou Bia, at 2,700 m elevation, is the highest peak in the province, and the highest in Laos. The capital city is at an elevation of about 1,000 m above mean sea level (AMSL), with Kham District in a low-laying basin at an elevation of about 600 m AMSL. Protected areas.

Geographic entities mentioned:
surface_form: Phou Bia
instance_of: Mountain
countries: Laos
coordinates: lat: 18.983333333333
lon: 103.13333333333
Radio Majevica is a Bosnian local commercial radio station, broadcasting from Lopare, Bosnia and Herzegovina. This radio station broadcasts a variety of programs such as folk and turbo-folk music with local news. Program is mainly produced in Serbian language at one FM frequency (Lopare) and it is available in Lopare near Bijeljina as well as in nearby municipalities in Semberija area.

Geographic entities mentioned:
surface_form: Semberija
instance_of: Landform
countries: Bosnia and Herzegovina
coordinates: lat: 44.80083333
lon: 19.21361111
Her works in Chicago include the Equitable Building. De Blois joined Neuhaus & Taylor (now known as 3-D International) in Houston in 1974. In 1980, she began teaching at the University of Texas School of Architecture, and was a faculty member until 1993. She died at age 92 in Chicago, and had her ashes scattered on Lake Michigan.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Topography. There is extensive topographic variation in Mesoamerica, ranging from the high peaks circumscribing the Valley of Mexico and within the central Sierra Madre mountains to the low flatlands of the northern Yucatán Peninsula. The tallest mountain in Mesoamerica is Pico de Orizaba, a dormant volcano located on the border of Puebla and Veracruz. Its peak elevation is 5,636 m (18,490 ft).

Geographic entities mentioned:
surface_form: Valley of Mexico
instance_of: Valley
countries: Mexico
coordinates: lat: 19.66666667
lon: -98.86666667
Topography. There is extensive topographic variation in Mesoamerica, ranging from the high peaks circumscribing the Valley of Mexico and within the central Sierra Madre mountains to the low flatlands of the northern Yucatán Peninsula. The tallest mountain in Mesoamerica is Pico de Orizaba, a dormant volcano located on the border of Puebla and Veracruz. Its peak elevation is 5,636 m (18,490 ft).

Geographic entities mentioned:
surface_form: Pico de Orizaba
instance_of: Mountain
countries: Mexico
coordinates: lat: 19.03
lon: -97.27
This volcano, which retains its Nahuatl name, is located 70 km (43 mi) southeast of Mexico City. Other volcanoes of note include Tacana on the Mexico–Guatemala border, Tajumulco and Santamaría in Guatemala, Izalco in El Salvador, Arenal in Costa Rica, Cerro Negro, along with Concepción and Maderas on Ometepe, which is an island formed by both volcanoes rising out of Lake Cocibolca in Nicaragua.

Geographic entities mentioned:
surface_form: Arenal
instance_of: Mountain
countries: Costa Rica
coordinates: lat: 10.463333333333
lon: -84.703333333333
surface_form: Cerro Negro
instance_of: Mountain
countries: Nicaragua
coordinates: lat: 12.5078224
lon: -86.7032877
surface_form: Maderas
instance_of: Mountain
countries: Nicaragua
coordinates: lat: 11.445833333333
lon: -85.515
With an area of 8,264 km2 (3,191 sq mi), Lake Cocibolca in Nicaragua is the largest lake in Mesoamerica, and second largest in all Latin America. Lake Chapala is Mexico's largest freshwater lake, but Lake Texcoco is perhaps most well known as the location upon which Tenochtitlan, capital of the Aztec Empire, was founded.

Geographic entities mentioned:
surface_form: Lake Chapala
instance_of: Lake
countries: Mexico
coordinates: lat: 20.333333333333
lon: -103
surface_form: Lake Texcoco
instance_of: Lake
countries: Mexico
coordinates: lat: 19.5
lon: -98.99
Lake Chapala is Mexico's largest freshwater lake, but Lake Texcoco is perhaps most well known as the location upon which Tenochtitlan, capital of the Aztec Empire, was founded. Lake Petén Itzá, in northern Guatemala, is notable as where the last independent Maya city, Tayasal (or Noh Petén), held out against the Spanish until 1697.

Geographic entities mentioned:
surface_form: Lake Petén Itzá
instance_of: Lake
countries: Guatemala
coordinates: lat: 16.983333333333
lon: -89.8
Lake Petén Itzá, in northern Guatemala, is notable as where the last independent Maya city, Tayasal (or Noh Petén), held out against the Spanish until 1697. Other large lakes include Lake Atitlán, Lake Izabal, Lake Güija, Lemoa and Lake Xolotlan. Biodiversity.

Geographic entities mentioned:
surface_form: Lake Izabal
instance_of: Lake
countries: Guatemala
coordinates: lat: 15.5
lon: -89.166666666667
Background. Sonoma Raceway, formerly Sears Point Raceway and Infineon Raceway is a road course and drag strip located on the landform known as Sears Point in the southern Sonoma Mountains in Sonoma, California, USA. The road course features 12 turns on a hilly course with of total elevation change.

Geographic entities mentioned:
surface_form: Sears Point
instance_of: Landform
countries: United States
coordinates: lat: 38.151111111111
lon: -122.44777777778
He is married to fellow actor and &quot;People for Education&quot; executive director Annie Kidder, who is the sister of Margot Kidder. Peterson and his wife live in Toronto, Ontario, with their two daughters, although he still frequents his home province of Saskatchewan, where he owns a cottage on Katepwa Lake in the Qu'Appelle Valley near his hometown. Awards.

Geographic entities mentioned:
surface_form: Katepwa Lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.6833
lon: -103.617
Oberaargau. The Oberaargau is the region that encompasses the upper watershed of the Aar River in the canton of Bern in Switzerland. On the north, lie the Jura Mountains, and on the south the hills leading to the Emmental. Administratively, the Oberaargau forms a district within the &quot;region&quot; Emmental-Oberaargau of the canton of Bern.

Geographic entities mentioned:
surface_form: Emmental
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.91922
lon: 7.77868
It is surrounded by the cantons of Solothurn, Aargau, and Lucerne. It is connected to the rest of the canton of Bern only in the south, where it borders on the Emmenthal. The Oberaargau lies on the Swiss Plateau between the large population centers of Bern and Zürich and has therefore become a major thoroughfare for traffic running both east and west and north and south.

Geographic entities mentioned:
surface_form: Swiss Plateau
instance_of: Plateau
countries: Switzerland
coordinates: lat: 47.1167
lon: 7.36667
The corner of Vitosha and Patriarch Evtimiy boulevards, so called the Pharmacy (), is a popular place for meetings. The boulevard is named after Vitosha, the mountain near Sofia. It was an unadjusted street during the Ottoman rule of Bulgaria and acquired the name &quot;Vitoshka ulitsa&quot; (&quot;Vitosha Street&quot;) after the Liberation in 1883.

Geographic entities mentioned:
surface_form: Vitosha
instance_of: Mountain
countries: Bulgaria
coordinates: lat: 42.566666666667
lon: 23.283333333333
Arenig Fawr South Top. Arenig Fawr South Top is the twin top of Arenig Fawr in southern Snowdonia, North Wales. It is the second highest member of the Arenig range, being 18 m less than its twin. From here the south ridge continues into an area of rocky knolls and small tarns, where Arenig Fawr South Ridge Top can be found.

Geographic entities mentioned:
surface_form: Arenig Fawr
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.917125
lon: -3.745937
Põrmujärv. Põrmujärv is a lake northwest of Voru City, in the county of Voru in Estonia's south, close to the border with Latvia.

Geographic entities mentioned:
surface_form: põrmujärv
instance_of: Lake
countries: Estonia
coordinates: lat: 57.879215
lon: 26.9596125
Geography. The mountain is the highest peak (1,799 m) of the Ligurian Apennines. It overlooks and Val Nure, and the &quot;comuni&quot; of Santo Stefano d'Aveto (province of Genoa) and Ferriere (province of Piacenza). On the summit is the statue of Our Lady of Guadalupe, erected in 1947 and a TV communication system.

Geographic entities mentioned:
surface_form: Val Nure
instance_of: Valley
countries: Italy
coordinates: lat: 44.7
lon: 9.56667
Monte Maggiorasca. Monte Maggiorasca is a mountain on the border between Liguria and Emilia-Romagna, northern Italy. Geography. The mountain is the highest peak (1,799 m) of the Ligurian Apennines. It overlooks and Val Nure, and the &quot;comuni&quot; of Santo Stefano d'Aveto (province of Genoa) and Ferriere (province of Piacenza).

Geographic entities mentioned:
surface_form: maggiorasca
instance_of: Mountain
countries: Italy
coordinates: lat: 44.55
lon: 9.4833333333333
surface_form: monte maggiorasca
instance_of: Mountain
countries: Italy
coordinates: lat: 44.55
lon: 9.4833333333333
Sydney E. Hutchinson of Philadelphia, Pennsylvania purchased the land to be called Foshalee Plantation between 1910 and 1914. The land lay west of Foshalee Slough, a swampy lowland extending from the eastern edge of Lake Iamonia. The purchase was for several miles of property to the east of the lake as well as to the north and south. Eventually Hutchinson would extend Foshalee to.

Geographic entities mentioned:
surface_form: Lake Iamonia
instance_of: Lake
countries: United States
coordinates: lat: 30.633119444444
lon: -84.177672222222
Beyond Shrewsbury, and especially beyond Llangollen, the work often involved building a highway from scratch. Notable features of this section of the route include the Waterloo Bridge across the River Conwy at Betws-y-Coed, the ascent from there to Capel Curig and then the descent from the Nant Ffrancon Pass towards Bangor.

Geographic entities mentioned:
surface_form: Nant Ffrancon Pass
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.1484
lon: -4.0414
Lake Henry (Codington County, South Dakota). Lake Henry is a natural lake in South Dakota, in the United States. Lake Henry takes its name from Henry, South Dakota, which was named for J. E. Henry, an early settler.

Geographic entities mentioned:
surface_form: lake henry
instance_of: Lake
countries: United States
coordinates: lat: 44.328333333333
lon: -97.485555555556
surface_form: lake henry
instance_of: Lake
countries: United States
coordinates: lat: 27.3237
lon: -81.3837
surface_form: lake henry
instance_of: Lake
countries: United States
coordinates: lat: 28.0928
lon: -81.6673
surface_form: lake henry (codington county, south dakota)
instance_of: Lake
countries: United States
coordinates: lat: 44.8532859
lon: -97.4790912
surface_form: lake henry
instance_of: Lake
countries: United States
coordinates: lat: 45.90222222
lon: -95.37611111
surface_form: lake henry
instance_of: Lake
countries: United States
coordinates: lat: 44.288888888889
lon: -93.815555555556
Lake Henry (Codington County, South Dakota). Lake Henry is a natural lake in South Dakota, in the United States. Lake Henry takes its name from Henry, South Dakota, which was named for J. E. Henry, an early settler.

Geographic entities mentioned:
surface_form: lake henry
instance_of: Lake
countries: United States
coordinates: lat: 44.328333333333
lon: -97.485555555556
surface_form: lake henry
instance_of: Lake
countries: United States
coordinates: lat: 27.3237
lon: -81.3837
surface_form: lake henry
instance_of: Lake
countries: United States
coordinates: lat: 28.0928
lon: -81.6673
surface_form: lake henry
instance_of: Lake
countries: United States
coordinates: lat: 44.8532859
lon: -97.4790912
surface_form: lake henry
instance_of: Lake
countries: United States
coordinates: lat: 45.90222222
lon: -95.37611111
surface_form: lake henry
instance_of: Lake
countries: United States
coordinates: lat: 44.288888888889
lon: -93.815555555556
The St. Mark's School () is an Anglican co-educated band 1 school located in the Eastern District of Hong Kong. It was admitted to the Grant School council in 1955 after the school being established in 1948. History. St. Mark's School was founded at Glenealy in Central in 1949, first known as St. Paul's English PM School. The founding principal was Mr. Leslie Wah-Leung Chung () (1917–2009)
.

Geographic entities mentioned:
surface_form: Glenealy
instance_of: Valley
countries: People's Republic of China
coordinates: lat: 22.278235
lon: 114.153957
Mount Victoria (Bow Range). __NOTOC__
Mount Victoria, is a mountain on the border between British Columbia and Alberta in the Canadian Rockies. It is located just northeast of Lake O'Hara in Yoho National Park and is also part of Banff National Park and is on the Continental Divide (which is the definition of the interprovincial boundary in this region).

Geographic entities mentioned:
surface_form: Lake O'Hara
instance_of: Lake
countries: Canada
coordinates: lat: 51.355902777778
lon: -116.33044444444
The mountain has two peaks, the south being the highest while the north peak is slightly lower at. The mountain is located on the western buttress of Abbot Pass while Mount Lefroy lies on the eastern side. The mountain was named by J. Norman Collie in 1897 for Queen Victoria. The first successful ascent was made in 1897 by J. Norman Collie, Arthur Michael, Charles Fay, and Peter Sarbach. Geology.

Geographic entities mentioned:
surface_form: Mount Lefroy
instance_of: Mountain
countries: Canada
coordinates: lat: 51.36222222222222
lon: -116.27972222222222
Mount Victoria (Bow Range). __NOTOC__
Mount Victoria, is a mountain on the border between British Columbia and Alberta in the Canadian Rockies. It is located just northeast of Lake O'Hara in Yoho National Park and is also part of Banff National Park and is on the Continental Divide (which is the definition of the interprovincial boundary in this region).

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: mount victoria
instance_of: Mountain
countries: Canada
coordinates: lat: 51.37694444444445
lon: -116.30666666666667
Mount Victoria (Bow Range). __NOTOC__
Mount Victoria, is a mountain on the border between British Columbia and Alberta in the Canadian Rockies. It is located just northeast of Lake O'Hara in Yoho National Park and is also part of Banff National Park and is on the Continental Divide (which is the definition of the interprovincial boundary in this region).

Geographic entities mentioned:
surface_form: mount victoria (bow range)
instance_of: Mountain
countries: Canada
coordinates: lat: 51.37694444444445
lon: -116.30666666666667
Norman Collie in 1897 for Queen Victoria. The first successful ascent was made in 1897 by J. Norman Collie, Arthur Michael, Charles Fay, and Peter Sarbach. Geology. Mount Victoria is composed of sedimentary rock laid down during the Cambrian period. Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny. Climate.

Geographic entities mentioned:
surface_form: mount victoria
instance_of: Mountain
countries: Canada
coordinates: lat: 51.37694444444445
lon: -116.30666666666667
Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny. Climate. Based on the Köppen climate classification, Mount Victoria is located in a subarctic climate zone with cold, snowy winters, and mild summers. Winter temperatures can drop below −20 °C with wind chill factors below −30 °C.

Geographic entities mentioned:
surface_form: mount victoria
instance_of: Mountain
countries: Canada
coordinates: lat: 51.37694444444445
lon: -116.30666666666667
They did not explain the origin of the specific epithet, but &quot;petro-&quot; is derived from the Greek for rock and &quot;-phila&quot; from the Greek for beloved, so that &quot;petrophila&quot; means &quot;rock-loving&quot;. The plants described by Coville and Morton were growing in a north facing vertical limestone wall in Titus Canyon in Death Valley, California.

Geographic entities mentioned:
surface_form: Death Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.45693888888889
lon: -116.86528055555556
The lake is close to the N4 primary road. Hydrology. Lough Owel and Lough Ennell are two of many lakes that form the River Brosna drainage basin. The Brosna is a tributary of the Shannon, flowing through Mullingar and Kilbeggan, both in Westmeath, and from there through the town of Clara (County Offaly) into the Shannon.

Geographic entities mentioned:
surface_form: Lough Ennell
instance_of: Lake
countries: Ireland
coordinates: lat: 53.45
lon: -7.4166666666667
surface_form: lough owel
instance_of: Lake
countries: Ireland
coordinates: lat: 53.573055555556
lon: -7.3883333333333
Lough Owel. Lough Owel () is a mesotrophic lough in the Midlands of Ireland, situated north of Mullingar, the county town of Westmeath. It has a maximum depth of. Water from Lough Owel feeds the Royal Canal, a canal crossing Ireland from Dublin to the River Shannon. The lake is close to the N4 primary road. Hydrology.

Geographic entities mentioned:
surface_form: lough owel
instance_of: Lake
countries: Ireland
coordinates: lat: 53.573055555556
lon: -7.3883333333333
St Loman was a hermit on the island, where he was said to have subsisted on a diet of wild alexanders (&quot;Smyrnium olusatrum&quot;). The other three islands are Srudarra Island, Lady's Island and Carrickphilbin Island. The Viking chieftain Turgesius is said to have been drowned in Lough Owel by Máel Sechnaill mac Maíl Ruanaid in 845. Natural history.

Geographic entities mentioned:
surface_form: lough owel
instance_of: Lake
countries: Ireland
coordinates: lat: 53.573055555556
lon: -7.3883333333333
At low elevations, rain is unpredictable at any time of year, although the showers tend to be shorter in summer. The uplands of Wales have most rain, normally more than 50 days of rain during the winter months (December to February), falling to around 35 rainy days during the summer months (June to August). Annual rainfall in Snowdonia averages between (Blaenau Ffestiniog) and (Snowdon's summit).

Geographic entities mentioned:
surface_form: Snowdon
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.068863888889
lon: -4.0755888888889
The Hebrides experience on average 35 days of gale a year (a day where there are gale-force winds) while inland areas in England and Wales receive fewer than 5 days of gale a year. Areas of high elevation tend to have higher wind speeds than low elevations, and Great Dun Fell in Cumbria (at) averaged 114 days of gale a year during the period 1963 to 1976.

Geographic entities mentioned:
surface_form: Great Dun Fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.683111111111
lon: -2.4513194444444
The mountains of Wales, Scotland, the Pennines in Northern England and the moors of South West England are the wettest parts of the country, and in some of these places as much as of rain can fall annually, making these locations some of the wettest in Europe. The wettest spot in the United Kingdom is Crib Goch, in Snowdonia, which averaged rain over a 30 year period.

Geographic entities mentioned:
surface_form: Crib Goch
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.075541666667
lon: -4.0535138888889
Maximum temperatures. Below is a list of the highest and lowest daily maximum temperatures recorded in the UK. This is in accordance with the Met Office, hence readings from the Cairn Gorm station are not on this list. Minimum temperatures. Below is a list of the highest and lowest daily minimum temperatures recorded in the UK.

Geographic entities mentioned:
surface_form: Cairn Gorm
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.116714
lon: -3.644477
Minimum temperatures. Below is a list of the highest and lowest daily minimum temperatures recorded in the UK. This is in accordance with the met office, hence readings from the Cairn Gorm station are not on this list. Climate change. Central estimates produced by the Met Office predict average annual temperature to increase by 2 °C and the warmest summer day to increase by 3 °C by the 2050s.

Geographic entities mentioned:
surface_form: Cairn Gorm
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.116714
lon: -3.644477
Climate. Stirling has a borderline oceanic climate/warm-summer mediterranean climate (Cfb/Csb). It experiences pleasant, relatively summers & quite cool, rainy winters. Owing to its location near Mount Lofty, Stirling is the wettest place in South Australia, receiving an average of 1,107 millimetres (43.6 inches) of rain per year&mdash;more than twice the average of Adelaide.

Geographic entities mentioned:
surface_form: Mount Lofty
instance_of: Mountain
countries: Australia
coordinates: lat: -34.966666666667
lon: 138.7
Greenland Dock. Greenland Dock is the oldest of London's riverside wet docks, located in Rotherhithe area of the London Borough of Southwark. It used to be part of the Surrey Commercial Docks, most of which have by now been filled in.

Geographic entities mentioned:
surface_form: Surrey Commercial Docks
instance_of: Body of water
countries: United Kingdom
coordinates: lat: 51.495
lon: -0.038333333333333
The Company built a series of additional docks and two new timber ponds to the north while rival companies built additional docks, leading to the jumble of harbours, canals and timber ponds. In 1865, the company merged with the neighbouring Surrey Docks to form the Surrey Commercial Docks, controlling some 80% of London's timber trade.

Geographic entities mentioned:
surface_form: Surrey Commercial Docks
instance_of: Body of water
countries: United Kingdom
coordinates: lat: 51.495
lon: -0.038333333333333
Coshocton County, Ohio. Coshocton County is a county located in the U.S. state of Ohio. As of the 2020 census, the population was 36,612. Its county seat and largest city is Coshocton. The county lies within the Appalachian region of the state. The county was formed on January 31, 1810, from portions of Muskingum and Tuscarawas Counties and later organized in 1811.

Geographic entities mentioned:
surface_form: Appalachian
instance_of: Plateau
countries: United States
coordinates: lat: 40
lon: -78
Oliver Wheeler. Sir Edward Oliver Wheeler MC (April 18, 1890 &ndash; March 19, 1962) was a Canadian surveyor, mountain climber and soldier. Wheeler participated in the first topographical survey of Mount Everest in 1921. As a brigadier in the British Army he was appointed Surveyor General of India in 1941. He was knighted for the work he did surveying India.

Geographic entities mentioned:
surface_form: Mount Everest
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.988055555555555
lon: 86.925
Wheeler participated in the first topographical survey of Mount Everest in 1921. As a brigadier in the British Army he was appointed Surveyor General of India in 1941. He was knighted for the work he did surveying India. He was an accomplished mountain climber and on the 1921 expedition was one of the team to reach the 7000-metre North Col. Early life.

Geographic entities mentioned:
surface_form: North Col
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 28.015833333333
lon: 86.925