Sarmila/GeoWiki-Features huggingface dataset:
Adults are on wing from April to May and from June to August. The larvae feed on reed sweet-grass (&quot;Glyceria maxima&quot;), mining the leaves of their host plant. Larvae can be found from April to May and again from July to August. Distribution. It is found from Fennoscandia and the Baltic region to Belgium, the Alps and Hungary and from Ireland to Romania.

Geographic entities mentioned:
surface_form: Fennoscandia
instance_of: Landform
countries: Norway
Sweden
Finland
Russia
Russian Empire
Soviet Union
coordinates: lat: 63
lon: 17
Gaz Khan. Gaz Khan or Goz Khun is a village in the Wakhan in Badakhshan Province in north-eastern Afghanistan. It is located at the confluence of the Panj River and Wakhan River, The village is the starting point for treks into the Great Pamir. Gaz Khan is inhabited by Wakhi people. The population of the village (2003) is 149.

Geographic entities mentioned:
surface_form: Great Pamir
instance_of: Valley
countries: Afghanistan
Tajikistan
coordinates: lat: 37.4
lon: 73.61666667
Fin Cop. Fin Cop is a hill and an associated Iron Age hill fort in Monsal Dale, close to Ashford in the Water in Derbyshire, England. The fort shows evidence of hurried construction, indicating a defensive response to a real threat, rather than the more usual assumption that such forts were a display of status and prestige.

Geographic entities mentioned:
surface_form: Monsal Dale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.244719444444
lon: -1.7317194444444
surface_form: fin cop
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.2358
lon: -1.73694
Fin Cop. Fin Cop is a hill and an associated Iron Age hill fort in Monsal Dale, close to Ashford in the Water in Derbyshire, England. The fort shows evidence of hurried construction, indicating a defensive response to a real threat, rather than the more usual assumption that such forts were a display of status and prestige.

Geographic entities mentioned:
surface_form: fin cop
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.2358
lon: -1.73694
The fort shows evidence of hurried construction, indicating a defensive response to a real threat, rather than the more usual assumption that such forts were a display of status and prestige. The hillfort, along with an adjacent bowl barrow, lime kiln and quarry, constitutes a Scheduled Ancient Monument.

Geographic entities mentioned:
surface_form: barrow
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5858
lon: -3.19703
On Faxian's way back to China, after a two-year stay in Sri Lanka, a violent storm drove his ship onto an island, probably Java. After five months there, Faxian took another ship for southern China, but again it was blown off course and he ended up landing at Mount Lao in what is now Shandong in northern China, east of the city of Qingdao.

Geographic entities mentioned:
surface_form: Mount Lao
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 36.191666666667
lon: 120.59166666667
Birg (Bernese Alps). Birg (2,684 m) is a summit of the Bernese Alps, overlooking the valley of Lauterbrunnen in the canton of Bern. It lies on the east flank of the Schilthorn, above the village of Mürren. In winter Birg is part of a ski area and several cable car stations are located on its summit. Birg is also an intermediate station between Mürren and of the Schilthorn.

Geographic entities mentioned:
surface_form: Schilthorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.557222222222
lon: 7.8352777777778
Birg is also an intermediate station between Mürren and of the Schilthorn. Birg appears as the ski station nearest to Blofeld's alpine headquarters Piz Gloria in the James Bond film &quot;On Her Majesty's Secret Service&quot;.&quot; It is first seen from a helicopter, but also has a scene set on it later on.

Geographic entities mentioned:
surface_form: first
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.50486111
lon: 7.64305556
surface_form: birg
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.5617
lon: 7.85583
surface_form: first
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.6608
lon: 8.05469
Birg (Bernese Alps). Birg (2,684 m) is a summit of the Bernese Alps, overlooking the valley of Lauterbrunnen in the canton of Bern. It lies on the east flank of the Schilthorn, above the village of Mürren. In winter Birg is part of a ski area and several cable car stations are located on its summit. Birg is also an intermediate station between Mürren and of the Schilthorn.

Geographic entities mentioned:
surface_form: birg
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.5617
lon: 7.85583
Birg (Bernese Alps). Birg (2,684 m) is a summit of the Bernese Alps, overlooking the valley of Lauterbrunnen in the canton of Bern. It lies on the east flank of the Schilthorn, above the village of Mürren. In winter Birg is part of a ski area and several cable car stations are located on its summit. Birg is also an intermediate station between Mürren and of the Schilthorn.

Geographic entities mentioned:
surface_form: birg
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.5617
lon: 7.85583
surface_form: schilthorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.557222222222
lon: 7.8352777777778
Sydenham Ward. Sydenham (commonly referred to as &quot;Sydenham Ward&quot;) is a central business district located in Kingston, Ontario, Canada. The Sydenham district for census purposes is bounded by Lake Ontario to the south and east, by Princess Street to the north and Barrie Street to the west.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
Mchenga conophoros. &quot;Mchenga conophoros&quot; is a species of fish in the family Cichlidae. It is endemic to Lake Malawi, where it has been collected around the Nankumba Peninsula in Malawi. Its natural habitat is freshwater lakes.

Geographic entities mentioned:
surface_form: Lake Malawi
instance_of: Lake
countries: Malawi
Mozambique
Tanzania
coordinates: lat: -12.183333333333
lon: 34.366666666667
Three Buttes. The Three Buttes, el., are buttes or small, flat-topped hills northwest of Lodge Pole, Montana in Blaine County, Montana.

Geographic entities mentioned:
surface_form: three buttes
instance_of: Landform
countries: United States
coordinates: lat: 48.1761
lon: -108.75
Bridge of Cally. Bridge of Cally is a small village in Kirkmichael parish, Perth and Kinross, Scotland. It sits at the junction of three glens, Glenshee, Strathardle and Glenericht and is centred round the bridge over the River Ardle before it joins the Black Water (which drains Glen Shee as Shee Water) to form the River Ericht.

Geographic entities mentioned:
surface_form: Glen Shee
instance_of: Valley
countries: United Kingdom
coordinates: lat: 56.8
lon: -3.4333333333333
Hercules Glades Wilderness. The Hercules Glades Wilderness is a wilderness area in Taney County in the Ozarks of southwest Missouri. The United States Congress designated it a wilderness in 1976, making it the oldest wilderness area in Missouri.

Geographic entities mentioned:
surface_form: Ozarks
instance_of: Plateau
countries: United States
coordinates: lat: 37.1822
lon: -92.5159
Ilija Čarapić. Ilija Čarapić (,), was the first Mayor of Belgrade, Serbia. He was born in 1792 in Beli Potok, near Avala, and died in 1844. He was son of the Voyvode Vasa Čarapić and the brother-in-law of Karađorđe, appointed as Voyvode or Duke of Grocka when he was only 18 years old after his uncle, Voyvode Tanasije Čarapić, who died in Prahovo, near Negotin.

Geographic entities mentioned:
surface_form: Avala
instance_of: Mountain
countries: Serbia
coordinates: lat: 44.690555555556
lon: 20.514166666667
The species can be found in Europe. Observations on the platform INaturalist spread as far north as Stockholm, Denmark, and Liverpool. The eastern end are the Ural Mountains. The southern edge lies in southern France and the Po Valley. The western edge lies in Cornwall and Brittany. The habitat is tied to the presence of figworts, which are ponds, streams or hedge banks. Naming.

Geographic entities mentioned:
surface_form: Po Valley
instance_of: Valley
countries: Italy
coordinates: lat: 45.330277777778
lon: 9.7988888888889
The small, now uninhabited (borough) of Solaro is situated north of the main settlement. Territory. The territory of Gottolengo lies within the Po Valley. The &quot;comune&quot; is positioned near the borders of the Province of Cremona and the Province of Mantua and falls within the Eastern Bassa Bresciana, the flat lowland area in the southeastern part of the province.

Geographic entities mentioned:
surface_form: Po Valley
instance_of: Valley
countries: Italy
coordinates: lat: 45.330277777778
lon: 9.7988888888889
In the immediate post-World War II years, the municipality’s population peaked at residents. During this period, even the now-deserted &quot;frazione&quot; of Solaro housed around 1,500 people in vast &quot;cascine a corte&quot; typical of the Po Valley, as well as some public buildings.

Geographic entities mentioned:
surface_form: Po Valley
instance_of: Valley
countries: Italy
coordinates: lat: 45.330277777778
lon: 9.7988888888889
This spurred significant funding and tax incentives, fostering modern industrial growth and diversification. Gottolengo is famous for its chestnut preserves (a sweet made with chestnuts from Val Camonica) and is the birthplace of Brescian quince jam. A family-run factory, operating since the early 20th century, produces mustards and assorted sauces.

Geographic entities mentioned:
surface_form: Val Camonica
instance_of: Valley
countries: Italy
coordinates: lat: 46.0075
lon: 10.3475
Urban transportation. The municipality lies within the local public transport subnetwork of the Province of Brescia, encompassing the Lower Brescia Plain, the Sebino area, and Franciacorta. Intercity transportation is provided by buses operated by the Trasporti Brescia Sud consortium, composed of SIA, SAIA Trasporti and APAM. Sports.

Geographic entities mentioned:
surface_form: Sebino
instance_of: Lake
countries: Italy
coordinates: lat: 45.711666666667
lon: 10.071944444444
SS Robert Wallace. SS &quot;Robert Wallace&quot; was a wooden-hulled American bulk freighter that served on the Great Lakes of North America from her construction in 1882 to her sinking in 1902 on Lake Superior near the town of Palmers, St. Louis County, Minnesota, United States.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
It is known for its extraordinary biodiversity and endemism. Geography. La Amistad International Park is equally split between Costa Rica and Panama, as part of the former &quot;La Amistad Reserves&quot;. The park protects a large part of the Cordillera de Talamanca mountain range, including the highest point in Costa Rica, Cerro Chirripó.

Geographic entities mentioned:
surface_form: Cerro Chirripó
instance_of: Mountain
countries: Costa Rica
coordinates: lat: 9.4840833333333
lon: -83.488666666667
By 1919, White had grown tired of film serials and signed with Fox Film Corporation with the ambition to appear in dramatic roles, including J. Searle Dawley's A Virgin Paradise, filmed near Harrington Sound in the British Imperial fortress colony of Bermuda, 640 miles off North Carolina where Searle had previously filmed The Relief of Lucknow and For Valour in 1912.

Geographic entities mentioned:
surface_form: Harrington Sound
instance_of: Lake
countries: United Kingdom
coordinates: lat: 32.329166666667
lon: -64.723333333333
James Bule. James Bule is a Vanuatuan politician and a member of the Parliament of Vanuatu from Ambae as a member of the People Unity Development Party. He was Minister of Justice and Community Services briefly in 2023.

Geographic entities mentioned:
surface_form: Ambae
instance_of: Mountain
countries: Vanuatu
coordinates: lat: -15.4
lon: 167.83333333333
and five churches. Parks and recreation. Twenty-four kilometres north of Carlyle on Highway 9, in the heart of Moose Mountain Uplands, is Moose Mountain Provincial Park, the most significant tourist attraction in the region. The park features Kenosee Lake, Kenosee Superslides, golfing, mini-golf, the Moose Mountain Chalet, camping, hiking, fishing, and many more activities.

Geographic entities mentioned:
surface_form: Kenosee Lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.8167
lon: -102.283
Beaverton, Ontario. Beaverton is a community in Brock Township in the Regional Municipality of Durham, Ontario, Canada. It is located on the eastern shore of Lake Simcoe at the mouth of the Beaver River. History. Beaverton was first settled in 1822.

Geographic entities mentioned:
surface_form: Lake Simcoe
instance_of: Lake
countries: Canada
coordinates: lat: 44.436666666667
lon: -79.339166666667
Detroit–Shoreway. Detroit–Shoreway is a neighborhood on the West Side of Cleveland, in the U.S. state of Ohio. Detroit–Shoreway consists of the streets between Lake Erie and Interstate 90, from West 85th to West 45th streets. Gordon Square. The retail hub of Detroit–Shoreway is Gordon Square, a series of retail buildings on the four corners of Detroit Avenue and West 65th Street. Named for W.J.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
Mount Ephraim (Vermont). Mount Ephraim is a mountain near Springfield, Vermont, U.S. and the highest land mass in the Precision Valley. It features one of several mysterious stone monuments that appear through the area.

Geographic entities mentioned:
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: mount ephraim
instance_of: Mountain
countries: United States
coordinates: lat: 43.2512
lon: -72.5143
Mount Ephraim (Vermont). Mount Ephraim is a mountain near Springfield, Vermont, U.S. and the highest land mass in the Precision Valley. It features one of several mysterious stone monuments that appear through the area.

Geographic entities mentioned:
surface_form: mount ephraim
instance_of: Mountain
countries: United States
coordinates: lat: 43.2512
lon: -72.5143
During its course through the city, the Onyar river is joined by the waters coming from the Monar or Conda irrigation channel (which in turn comes from the Ter river), a channel that used to irrigate the orchards in the &quot;Mercadal&quot; area. As it journeys further north, the river converges with the Güell and the Galligans rivers near the crossing with the railway.

Geographic entities mentioned:
surface_form: güell
instance_of: Watercourse
countries: Spain
coordinates: lat: 41.937917
lon: 2.791699
Finally, it merges into the Ter river near the Pedret neighborhood. Over the years, the Onyar and Güell rivers have been associated with notable flood events that have had a profound impact on the city. The period spanning from 1970 to 1985 was particularly devastating, resulting in significant material losses.

Geographic entities mentioned:
surface_form: güell
instance_of: Watercourse
countries: Spain
coordinates: lat: 41.937917
lon: 2.791699
surface_form: onyar
instance_of: Watercourse
countries: Spain
coordinates: lat: 41.970555555556
lon: 2.8394444444444
Onyar. The Onyar (; Spanish: Oñar; &quot;Undarius&quot; in Latin) is a Spanish river in Girona, Catalonia that begins at the Guilleries massif at the apex of the Catalan Transversal Range and the Pre-Coastal Range. It joins the Ter at the city of Girona, and crosses the city from south to north, separating the city into the old part (on the right side) and the more modern part (on the left side).

Geographic entities mentioned:
surface_form: oñar
instance_of: Watercourse
countries: Spain
coordinates: lat: 41.970555555556
lon: 2.8394444444444
surface_form: onyar
instance_of: Watercourse
countries: Spain
coordinates: lat: 41.970555555556
lon: 2.8394444444444
surface_form: undarius
instance_of: Watercourse
countries: Spain
coordinates: lat: 41.970555555556
lon: 2.8394444444444
Onyar. The Onyar (; Spanish: Oñar; &quot;Undarius&quot; in Latin) is a Spanish river in Girona, Catalonia that begins at the Guilleries massif at the apex of the Catalan Transversal Range and the Pre-Coastal Range. It joins the Ter at the city of Girona, and crosses the city from south to north, separating the city into the old part (on the right side) and the more modern part (on the left side).

Geographic entities mentioned:
surface_form: onyar
instance_of: Watercourse
countries: Spain
coordinates: lat: 41.970555555556
lon: 2.8394444444444
During its course through the city, the Onyar river is joined by the waters coming from the Monar or Conda irrigation channel (which in turn comes from the Ter river), a channel that used to irrigate the orchards in the &quot;Mercadal&quot; area. As it journeys further north, the river converges with the Güell and the Galligans rivers near the crossing with the railway.

Geographic entities mentioned:
surface_form: onyar
instance_of: Watercourse
countries: Spain
coordinates: lat: 41.970555555556
lon: 2.8394444444444
These floods are documented to have affected over 75% of the city, causing disruption to approximately 2000 commercial and industrial establishments, as well as damaging or destroying 500 vehicles
The river flows alongside a charming tourist destination known as the Onyar's houses (&quot;Casas del Onyar&quot; in Catalan), comprising a vibrant ensemble of homes that have become iconic subjects for postcards and tourist literature

Geographic entities mentioned:
surface_form: onyar
instance_of: Watercourse
countries: Spain
coordinates: lat: 41.970555555556
lon: 2.8394444444444
surface_form: onyar
instance_of: Watercourse
countries: Spain
coordinates: lat: 41.970555555556
lon: 2.8394444444444
Chender. Chender is a village in the Boumerdès Province in Kabylie, Algeria. Location. The village is surrounded by Chender River and Sebaou River, and the towns of Naciria and Bordj Menaïel.

Geographic entities mentioned:
surface_form: Sebaou River
instance_of: Watercourse
countries: Algeria
France
coordinates: lat: 36.9114
lon: 3.8543
The main features of the range formed before 34 million years ago, when the area was covered by the present ice sheet. Current models suggest that the East Antarctic ice sheet was formed from the glaciers that began sliding down the Gamburtsev range at the end of the Eocene. Vostok Subglacial Highlands form an east extension of Gamburtsev Subglacial Mountains.

Geographic entities mentioned:
surface_form: Vostok Subglacial Highlands
instance_of: Landform
coordinates: lat: -80
lon: 102
About 250-100 million years ago, the crust started to pull apart in a series of rifting events close to the east of this old root. A forked rift valley runs along the northern side of the mountains containing lakes Sovetskaya and 90East within it. This rifting warmed and rejuvenated the root, giving it the buoyancy to be lifted up to re-establish the mountains as an 800 km long massif.

Geographic entities mentioned:
surface_form: 90East
instance_of: Lake
coordinates: lat: -77.4
lon: 90
Mường Thanh Valley. The Mường Thanh Valley is a valley located in the Điện Biên Province of Northwestern Vietnam. The valley is approximately 20 km long by 5 km wide. A heart-shaped basin, the valley is surrounded by a region filled with jungles, rice paddies, and lakes. Located within the Mường Thanh Valley is the city of Điện Biên Phủ.

Geographic entities mentioned:
surface_form: mường thanh valley
instance_of: Valley
countries: Vietnam
coordinates: lat: 21.365967
lon: 103.008684
A heart-shaped basin, the valley is surrounded by a region filled with jungles, rice paddies, and lakes. Located within the Mường Thanh Valley is the city of Điện Biên Phủ. The capital of Điện Biên Province, Điện Biên Phủ, is famous as the site of a decisive battle in 1954 in which French forces were defeated by Việt Minh troops under general Võ Nguyên Giáp. Geography and location.

Geographic entities mentioned:
surface_form: mường thanh valley
instance_of: Valley
countries: Vietnam
coordinates: lat: 21.365967
lon: 103.008684
Geography and location. Located in the Điện Biên Province of Northwestern Vietnam, the Mường Thanh valley lies at the crossroads of many different modern political boundaries. Two other Vietnamese provinces border the Điện Biên Province, Lai Châu to the east and north, and Sơn La to the east and south.

Geographic entities mentioned:
surface_form: mường thanh valley
instance_of: Valley
countries: Vietnam
coordinates: lat: 21.365967
lon: 103.008684
The valley is located 420 kilometers away from capital Hanoi. The Mường Thanh Valley lies in a hilly, lush region. The valley runs north-south and is situated in the western portion of the Điện Biên Province, approximately 16 km from the border with Laos. Demography and culture. Approximately 40 percent of the inhabitants of the Điện Biên Province belong to the Tai ethnic minority group.

Geographic entities mentioned:
surface_form: mường thanh valley
instance_of: Valley
countries: Vietnam
coordinates: lat: 21.365967
lon: 103.008684
Many of the ethnic groups in Northern Vietnam are Chinese-descended. However the Thai, among other ethnic groups that inhabit the Mường Thanh Valley and the surrounding highland regions, are not Chinese-descended. The Thai, along with other ethnic groups that inhabit the Điện Biên Province, are largely independent and follow their own series of customs and traditions.

Geographic entities mentioned:
surface_form: mường thanh valley
instance_of: Valley
countries: Vietnam
coordinates: lat: 21.365967
lon: 103.008684
They were forced into the highlands by continuous invasions of the Mongoloid people of China. While the Thai are the largest single ethnic group in the Mường Thanh Valley, the Hmong, Dao, and Day ethnic groups also inhabit the valley. There is also a substantial population of the Vietnamese ethnic majority group, Kinh, in the city of Dien Bien Phu.

Geographic entities mentioned:
surface_form: mường thanh valley
instance_of: Valley
countries: Vietnam
coordinates: lat: 21.365967
lon: 103.008684
The valley was associated with Muang Then, a legendary land where the Tai peoples first settled after migrating southward from Yunnan around the time of the Kingdom of Nanzhao under their leader Khun Borom. Due to its location along the border with Laos and near the border with China, the Mường Thanh Valley and the surrounding region has had a long history of invasions and political change.

Geographic entities mentioned:
surface_form: mường thanh valley
instance_of: Valley
countries: Vietnam
coordinates: lat: 21.365967
lon: 103.008684
In the 15th century, the troops of Vietnamese Emperor Lê Lợi allied with the indigenous inhabitants to expel the Chinese Ming invaders. Three hundred years later, the Mường Thanh Valley came under the occupation of the Phe people from Laos. The Thai vigorously fought the Phe invaders and finally defeated them in 1751 with help from a peasant leader from Son Nam named Hoang Cong Chat.

Geographic entities mentioned:
surface_form: mường thanh valley
instance_of: Valley
countries: Vietnam
coordinates: lat: 21.365967
lon: 103.008684
The Thai vigorously fought the Phe invaders and finally defeated them in 1751 with help from a peasant leader from Son Nam named Hoang Cong Chat. Until French rule began, the inhabitants of the Mường Thanh Valley and many of Vietnam's other highland minority groups were quite isolated from the major lowland populations.

Geographic entities mentioned:
surface_form: mường thanh valley
instance_of: Valley
countries: Vietnam
coordinates: lat: 21.365967
lon: 103.008684
Until French rule began, the inhabitants of the Mường Thanh Valley and many of Vietnam's other highland minority groups were quite isolated from the major lowland populations. When the French arrived in the nineteenth century they began to consolidate rule and contact between highland regions such as Mường Thanh and the lowland regions increased.

Geographic entities mentioned:
surface_form: mường thanh
instance_of: Valley
countries: Vietnam
coordinates: lat: 21.365967
lon: 103.008684
This often led to conflict between the French and the minority groups because the natives did not trust the French. After independence from the French, the Mường Thanh Valley fell under the rule of the North Vietnamese government and the inhabitants were given a certain degree of autonomy as a compromise for accepting the rule of the central government in Hanoi. Natural life.

Geographic entities mentioned:
surface_form: mường thanh valley
instance_of: Valley
countries: Vietnam
coordinates: lat: 21.365967
lon: 103.008684
Natural life. Flowing through the Mường Thanh Valley is the Nam Rom River. The presence of the Nam Rom River in the valley makes the valley region highly fertile. Much of the natural environment of the Mường Thanh Valley is jungle. The non-urbanized land in the valley is now largely used for agriculture, namely rice growing. Economic development.

Geographic entities mentioned:
surface_form: mường thanh valley
instance_of: Valley
countries: Vietnam
coordinates: lat: 21.365967
lon: 103.008684
Much of the natural environment of the Mường Thanh Valley is jungle. The non-urbanized land in the valley is now largely used for agriculture, namely rice growing. Economic development. While the area surrounding the Mường Thanh Valley is largely rural and undeveloped, the valley itself is developed. The capital of the Điện Biên Province, the city of Dien Bien Phu, is located inside the valley.

Geographic entities mentioned:
surface_form: mường thanh valley
instance_of: Valley
countries: Vietnam
coordinates: lat: 21.365967
lon: 103.008684
This announcement came with a gift of around US$9500 to each commune in Dien Bien to build a commune hall to host visitors. These communes will showcase and introduce tourists to Thai culture. Trekking, mountain biking, and other nature-oriented tourist activities are also being promoted in the Mường Thanh Valley. Additionally, a commercial airport is located in the Mường Thanh Valley.

Geographic entities mentioned:
surface_form: mường thanh valley
instance_of: Valley
countries: Vietnam
coordinates: lat: 21.365967
lon: 103.008684
These communes will showcase and introduce tourists to Thai culture. Trekking, mountain biking, and other nature-oriented tourist activities are also being promoted in the Mường Thanh Valley. Additionally, a commercial airport is located in the Mường Thanh Valley. The airport, located in Dien Bien Phu, offers flights to Hanoi. Rice farming also contributes to the local economy.

Geographic entities mentioned:
surface_form: mường thanh valley
instance_of: Valley
countries: Vietnam
coordinates: lat: 21.365967
lon: 103.008684
By late 1952 much of the Red River Delta was under Viet Minh control. Due to its proximity to supply routes from China, the Mường Thanh Valley region was vital to the survival and support of the Viet Minh. The French forces in Vietnam under General Henri Navarre sought to occupy Dien Bien Phu.

Geographic entities mentioned:
surface_form: mường thanh valley
instance_of: Valley
countries: Vietnam
coordinates: lat: 21.365967
lon: 103.008684
The siege of Dien Bien Phu began on March 13, 1954. By this date the Viet Minh had approximately 50,000 regular troops, 55,000 support troops in the area. They also had around 100,000 transport workers in Mường Thanh Valley area bringing in Chinese aid. The French garrison at Dien Bien Phu relied on air supply and on March 27 the Viet Minh had destroyed the French airfield.

Geographic entities mentioned:
surface_form: mường thanh valley
instance_of: Valley
countries: Vietnam
coordinates: lat: 21.365967
lon: 103.008684
The hindwings are pale fuscous basally with darker fuscous toward the margin. Adults have been recorded on wing from late May to late June and from late August to early November. Etymology. The species is named after the Molino Basin on Mount Lemmon where most of the type series was collected.

Geographic entities mentioned:
surface_form: Mount Lemmon
instance_of: Mountain
countries: United States
coordinates: lat: 32.443130555556
lon: -110.78843055556
Haddebyer Noor. Haddebyer Noor () is a lake – formerly a small arm of the Schlei inlet of the Baltic Sea – in Schleswig-Holstein, Germany. At an elevation of, its surface area is.

Geographic entities mentioned:
surface_form: haddebyer noor
instance_of: Lake
countries: Germany
coordinates: lat: 54.493333333333
lon: 9.5744444444444
R-17 Elbrus. The R-17 Elbrus (, named for Mount Elbrus), GRAU index 9K72 is a tactical ballistic missile, initially developed by the Soviet Union. It is also known by its NATO reporting name SS-1C Scud-B. The R-17 is one of several Soviet missiles to carry the reporting name Scud, and the most prolifically launched of the series, with a production run estimated at 7,000 (1960–1987).

Geographic entities mentioned:
surface_form: Mount Elbrus
instance_of: Mountain
countries: Russia
Soviet Union
Russian Empire
coordinates: lat: 43.35254
lon: 42.437875
The Taliban managed to capture part of the surviving stockpile during the fighting in the late 1990s, but due the poor state of the equipment and lack of trained personnel, only five missiles were fired after the summer of 1996. Following the United States invasion of Afghanistan in 2001, the remaining four functional launchers were scrapped in the Panjshir Valley in January 2005. Armenia.

Geographic entities mentioned:
surface_form: Panjshir Valley
instance_of: Valley
countries: Afghanistan
coordinates: lat: 35.266666666667
lon: 69.466666666667
See &quot;Fragaria&quot;. Distribution. &quot;F. cascadensis&quot; grows along the western slopes of the Oregon Cascades Mountains from the Columbia River south to Crater Lake, at elevations of about 3,000 feet up to tree line. It grows in sandy-clay loam soil of volcanic origin located in forest clearings and open alpine meadows. Cultivation. This species is not yet in cultivation.

Geographic entities mentioned:
surface_form: Crater Lake
instance_of: Lake
countries: United States
coordinates: lat: 42.943611111111
lon: -122.10666666667
Murlagan. Murlagan is a small hamlet located on the north shore of Loch Arkaig in Inverness-shire, Scottish Highlands and is in the Scottish council area of Highland. Murlagan, also called Murlaggan and Mhurlagain, is the location of the minor seat of Clan MacMillan. History. The Murlagan, chief of Clan MacMillan was tacksman to Cameron of Lochiel.

Geographic entities mentioned:
surface_form: Loch Arkaig
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.971989
lon: -5.158376
&ndash; &quot;Bygone Lochaber&quot;, Somerled MacMillan (1971)
Many generations of these MacMillans served the Camerons of Lochiel and worked land on Loch Arkaig, below the Mountain called Murlagan at the inland end of Loch Arkaig, which is near Fort William in the highlands of Scotland.

Geographic entities mentioned:
surface_form: Loch Arkaig
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.971989
lon: -5.158376
Examples of remote locations mapped using Tellurometer surveys are Adams Bluff, Churchill Mountains, Cook Mountains, Jacobsen Glacier, Mount Albright, Mount Predoehl, Mount Summerson, Sherwin Peak and Vogt Peak. The instrument penetrates haze and mist in daylight or darkness and has a normal range of 30–50 km but can extend up to 70 km.

Geographic entities mentioned:
surface_form: Mount Albright
instance_of: Mountain
coordinates: lat: -82.81667
lon: 155.1
surface_form: Mount Predoehl
instance_of: Mountain
coordinates: lat: -82.93333
lon: 163.18333
surface_form: Mount Summerson
instance_of: Mountain
coordinates: lat: -82.71667
lon: 155.08333
surface_form: Vogt Peak
instance_of: Mountain
coordinates: lat: -82.3666667
lon: 156.7333333
Description and history. The work is Hardy's largest, and took a year to complete. It depicts Oregon's landscape from west to east, including marine life, Oregon Coast Range, Willamette Valley, Cascade Range, and John Day Fossil Beds National Monument. The sculpture measures approximately x x, and is composed of eight panels with reddish-brown patina each measuring around x.

Geographic entities mentioned:
surface_form: Willamette Valley
instance_of: Valley
countries: United States
coordinates: lat: 44.9
lon: -123.1
Semthan. Semthan, also Semithan is a village 1 km north of Bijbehara in the Anantnag district of the Kashmir Valley in Jammu and Kashmir, India. It has an archaeological site, the ancient site of Chakradhar where cultural sequences were stratified, from the Neolithic to the Indo-Greek and Kushan periods. Excavations.

Geographic entities mentioned:
surface_form: Kashmir Valley
instance_of: Valley
countries: India
coordinates: lat: 34.0333
lon: 74.6667
It is the final section of the Southern Gas Corridor originating in Azerbaijan., capacity is 10 bcm per year. The natural gas originates in the second stage of the Shah Deniz (Azerbaijan) gas field development in the Azerbaijani section of Caspian Sea flowing through the South Caucasus Pipeline and the Trans Anatolian Pipeline (TANAP).

Geographic entities mentioned:
surface_form: Caspian Sea
instance_of: Body of water
Lake
countries: Iran
Russia
Kazakhstan
Azerbaijan
Turkmenistan
Russian Empire
Soviet Union
coordinates: lat: 42
lon: 50.5
&quot;Orecchiette&quot; is considered the signature pasta shape of Apulia, but there are many other shapes as well. These include &quot;cavatelli&quot;, &quot;capunti&quot; (typical of the Murgia plateau), &quot;troccoli&quot; (from the Daunia), &quot;lagane&quot; and &quot;sagne&quot;. &quot;Orecchiette&quot; is frequently combined with fried &quot;cime di rape&quot;.

Geographic entities mentioned:
surface_form: Murgia plateau
instance_of: Plateau
countries: Italy
coordinates: lat: 40.976
lon: 16.406
The grass pea (&quot;cicerchia&quot;) used to be popular in cookbooks of the 1600s, but has since fallen out of favor because the plant provides a limited yield and is toxic if eaten as a staple. In recent times the crop has been rediscovered and is cultivated in the Alta Murgia and the Salento. It is used in soups and stews. Seafood.

Geographic entities mentioned:
surface_form: Alta Murgia
instance_of: Plateau
countries: Italy
coordinates: lat: 40.976
lon: 16.406
Magnús J. Skaptason. Magnús J. Skaptason (born 4 February 1850, died Winnipeg, 8 March 1932) was an Icelandic priest and newspaper editor, noted for his activities among the Icelandic community in Canada. Life and thought. Magnús's mother was Anna Margrét (whose own father was Björn Ólsen of Þingeyri) and his father Dr. Jósep Skaptason (1802–75) of Hnausar in Vatnsdalur.

Geographic entities mentioned:
surface_form: Vatnsdalur
instance_of: Valley
countries: Iceland
coordinates: lat: 65.42472222
lon: -20.28666667
The California toad occurs from all of Northern California and down south into Baja California. There are scattered populations in isolated desert areas, such as in the Mojave Desert, but they generally do not occur in the desert areas from Death Valley southward. The habitats for the California toad range from woodland, grassland, and meadows in forest areas to backyards and parks in the suburbs.

Geographic entities mentioned:
surface_form: Death Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.45693888888889
lon: -116.86528055555556
Mount Waesche is a mountain of volcanic origin at the southern end of the Executive Committee Range in Marie Byrd Land, Antarctica. It is high, and stands southwest of Mount Sidley, the highest volcano in Antarctica. The mountain lies southwest of the Chang Peak caldera and is largely covered with snow and glaciers, but there are rock exposures on the southern and southwestern slopes.

Geographic entities mentioned:
surface_form: Mount Sidley
instance_of: Mountain
coordinates: lat: -77.04
lon: -126.1
It is high, and stands southwest of Mount Sidley, the highest volcano in Antarctica. The mountain lies southwest of the Chang Peak caldera and is largely covered with snow and glaciers, but there are rock exposures on the southern and southwestern slopes. The volcano may have been active as late as the Holocene, with tephra layers recovered from ice cores possibly originating from Mount Waesche.

Geographic entities mentioned:
surface_form: Chang Peak
instance_of: Mountain
coordinates: lat: -77.0667
lon: -126.633
surface_form: southern
instance_of: Mountain
coordinates: lat: -74.2
lon: -76.4667
It is one of 18 volcanoes in that region, which were active from the Oligocene to recent times. The origin of volcanic activity there has been correlated to the activity of a mantle plume underneath the crust. The region also includes the highest volcano in Antarctica, Mount Sidley, which reaches height. There may be as many as 138 volcanoes buried underneath the ice.

Geographic entities mentioned:
surface_form: Mount Sidley
instance_of: Mountain
coordinates: lat: -77.04
lon: -126.1
At least five parasitic vents lie on the volcano, with several aligned on radial fissure vents; they are cinder cones and scoria cones and have erupted cinder, lava and volcanic bombs. A long large radial dyke projects from Mount Waesche and is the only part of the edifice where hyaloclastic tuff crops out. The Bennet Saddle separates Mount Waesche from Mount Sidley to the northeast.

Geographic entities mentioned:
surface_form: Bennet Saddle
instance_of: Landform
coordinates: lat: -77.0833
lon: -126.433
surface_form: waesche
instance_of: Mountain
coordinates: lat: -77.166666666667
lon: -126.9
surface_form: mount waesche
instance_of: Mountain
coordinates: lat: -77.166666666667
lon: -126.9
Mount Waesche is largely covered with snow and features several alpine glaciers as well as a blue-ice area within the West Antarctic Ice Sheet; this blue-ice area has an extent of and a number of tephra layers crop out from the ice. Most of these tephra layers come from Mount Waesche, but some originate at Mount Takahe and Mount Berlin and their age ranges from 118,000 years to Holocene.

Geographic entities mentioned:
surface_form: Mount Takahe
instance_of: Mountain
coordinates: lat: -76.3
lon: -112.1
surface_form: Mount Berlin
instance_of: Mountain
coordinates: lat: -76.055
lon: -135.825
surface_form: takahe
instance_of: Mountain
coordinates: lat: -76.3
lon: -112.1
surface_form: waesche
instance_of: Mountain
coordinates: lat: -77.166666666667
lon: -126.9
surface_form: mount waesche
instance_of: Mountain
coordinates: lat: -77.166666666667
lon: -126.9
Geology. Mount Waesche is part of the Executive Committee Range, which from north to south includes Mount Hampton, Mount Cumming with the parasitic vent Annexstad Peak, Mount Hartigan, Mount Sidley with Doumani Peak and Chang Peak-Mount Waesche. These mountains are all volcanic and feature ice-filled calderas, and many are paired volcanoes.

Geographic entities mentioned:
surface_form: Mount Hampton
instance_of: Mountain
coordinates: lat: -76.483333333333
lon: -125.8
surface_form: Mount Cumming
instance_of: Mountain
coordinates: lat: -76.66667
lon: -126
surface_form: Annexstad Peak
instance_of: Mountain
coordinates: lat: -76.6833
lon: -125.867
surface_form: Mount Hartigan
instance_of: Mountain
coordinates: lat: -76.8
lon: -126
surface_form: Doumani Peak
instance_of: Mountain
coordinates: lat: -77.1167
lon: -126.05
surface_form: hampton
instance_of: Mountain
coordinates: lat: -76.483333333333
lon: -125.8
surface_form: mount hampton
instance_of: Mountain
coordinates: lat: -76.483333333333
lon: -125.8
surface_form: waesche
instance_of: Mountain
coordinates: lat: -77.166666666667
lon: -126.9
surface_form: mount waesche
instance_of: Mountain
coordinates: lat: -77.166666666667
lon: -126.9
surface_form: doumani
instance_of: Mountain
coordinates: lat: -85.8167
lon: -137.633
Eruption history. The development of Mount Waesche began in the Pliocene, and Plio-Pleistocene tephra layers found in the Southern Pacific Ocean may originate at Mount Waesche. It appears that volcanism in the Executive Committee Range moved southwards over time, beginning at Mount Hampton and eventually arriving at Mount Waesche which is the young volcanic centre of the range.

Geographic entities mentioned:
surface_form: hampton
instance_of: Mountain
coordinates: lat: -76.483333333333
lon: -125.8
surface_form: mount hampton
instance_of: Mountain
coordinates: lat: -76.483333333333
lon: -125.8
surface_form: waesche
instance_of: Mountain
coordinates: lat: -77.166666666667
lon: -126.9
surface_form: mount waesche
instance_of: Mountain
coordinates: lat: -77.166666666667
lon: -126.9
Mount Waesche. Mount Waesche is a mountain of volcanic origin at the southern end of the Executive Committee Range in Marie Byrd Land, Antarctica. It is high, and stands southwest of Mount Sidley, the highest volcano in Antarctica.

Geographic entities mentioned:
surface_form: waesche
instance_of: Mountain
coordinates: lat: -77.166666666667
lon: -126.9
surface_form: mount waesche
instance_of: Mountain
coordinates: lat: -77.166666666667
lon: -126.9
Mount Waesche. Mount Waesche is a mountain of volcanic origin at the southern end of the Executive Committee Range in Marie Byrd Land, Antarctica. It is high, and stands southwest of Mount Sidley, the highest volcano in Antarctica.

Geographic entities mentioned:
surface_form: waesche
instance_of: Mountain
coordinates: lat: -77.166666666667
lon: -126.9
surface_form: mount waesche
instance_of: Mountain
coordinates: lat: -77.166666666667
lon: -126.9
surface_form: southern
instance_of: Mountain
coordinates: lat: -74.2
lon: -76.4667
It is high, and stands southwest of Mount Sidley, the highest volcano in Antarctica. The mountain lies southwest of the Chang Peak caldera and is largely covered with snow and glaciers, but there are rock exposures on the southern and southwestern slopes. The volcano may have been active as late as the Holocene, with tephra layers recovered from ice cores possibly originating from Mount Waesche.

Geographic entities mentioned:
surface_form: waesche
instance_of: Mountain
coordinates: lat: -77.166666666667
lon: -126.9
surface_form: mount waesche
instance_of: Mountain
coordinates: lat: -77.166666666667
lon: -126.9
surface_form: active
instance_of: Landform
Body of water
coordinates: lat: -63.4167
lon: -56.1667
Name and research history. It was discovered by the United States Antarctic Service expedition on a flight on December 15, 1940, and named for Vice Admiral Russell R. Waesche, United States Coast Guard, member of the Antarctic Service Executive Committee. Field studies took place in 1999-2000 and 2018–2019. Geography and geomorphology.

Geographic entities mentioned:
surface_form: waesche
instance_of: Mountain
coordinates: lat: -77.166666666667
lon: -126.9
Field studies took place in 1999-2000 and 2018–2019. Geography and geomorphology. Mount Waesche lies in Marie Byrd Land, one of the most inaccessible areas of Antarctica. It is one of 18 volcanoes in that region, which were active from the Oligocene to recent times. The origin of volcanic activity there has been correlated to the activity of a mantle plume underneath the crust.

Geographic entities mentioned:
surface_form: waesche
instance_of: Mountain
coordinates: lat: -77.166666666667
lon: -126.9
surface_form: mount waesche
instance_of: Mountain
coordinates: lat: -77.166666666667
lon: -126.9
The region also includes the highest volcano in Antarctica, Mount Sidley, which reaches height. There may be as many as 138 volcanoes buried underneath the ice. Mount Waesche volcano is high. It is a double volcano, with the north-northeasterly Chang Peak caldera and the south-southwesterly Mount Waesche proper.

Geographic entities mentioned:
surface_form: waesche
instance_of: Mountain
coordinates: lat: -77.166666666667
lon: -126.9
surface_form: mount waesche
instance_of: Mountain
coordinates: lat: -77.166666666667
lon: -126.9
There may be as many as 138 volcanoes buried underneath the ice. Mount Waesche volcano is high. It is a double volcano, with the north-northeasterly Chang Peak caldera and the south-southwesterly Mount Waesche proper. The Chang Peak caldera is wide and the largest in Marie Byrd Land; Mount Waesche rises almost over and lies on the rim of the caldera.

Geographic entities mentioned:
surface_form: waesche
instance_of: Mountain
coordinates: lat: -77.166666666667
lon: -126.9
surface_form: mount waesche
instance_of: Mountain
coordinates: lat: -77.166666666667
lon: -126.9
The Chang Peak caldera is wide and the largest in Marie Byrd Land; Mount Waesche rises almost over and lies on the rim of the caldera. Mount Waesche is the more conspicuous peak and lava flows crop out on its southern and southwestern flank, while a wide caldera lies at its summit.

Geographic entities mentioned:
surface_form: waesche
instance_of: Mountain
coordinates: lat: -77.166666666667
lon: -126.9
surface_form: mount waesche
instance_of: Mountain
coordinates: lat: -77.166666666667
lon: -126.9
surface_form: southern
instance_of: Mountain
coordinates: lat: -74.2
lon: -76.4667
At least five parasitic vents lie on the volcano, with several aligned on radial fissure vents; they are cinder cones and scoria cones and have erupted cinder, lava and volcanic bombs. A long large radial dyke projects from Mount Waesche and is the only part of the edifice where hyaloclastic tuff crops out. The Bennet Saddle separates Mount Waesche from Mount Sidley to the northeast.

Geographic entities mentioned:
surface_form: waesche
instance_of: Mountain
coordinates: lat: -77.166666666667
lon: -126.9
surface_form: mount waesche
instance_of: Mountain
coordinates: lat: -77.166666666667
lon: -126.9
The Bennet Saddle separates Mount Waesche from Mount Sidley to the northeast. Mount Waesche is largely covered with snow and features several alpine glaciers as well as a blue-ice area within the West Antarctic Ice Sheet; this blue-ice area has an extent of and a number of tephra layers crop out from the ice.

Geographic entities mentioned:
surface_form: waesche
instance_of: Mountain
coordinates: lat: -77.166666666667
lon: -126.9
surface_form: mount waesche
instance_of: Mountain
coordinates: lat: -77.166666666667
lon: -126.9
Most of these tephra layers come from Mount Waesche, but some originate at Mount Takahe and Mount Berlin and their age ranges from 118,000 years to Holocene. Two particularly conspicuous tephra layers from Mount Waesche are known as the &quot;Great Wall&quot; and &quot;Yellow Wall&quot;. The volcano emerges through and is surrounded by the West Antarctic Ice Sheet.

Geographic entities mentioned:
surface_form: waesche
instance_of: Mountain
coordinates: lat: -77.166666666667
lon: -126.9
surface_form: mount waesche
instance_of: Mountain
coordinates: lat: -77.166666666667
lon: -126.9
Two particularly conspicuous tephra layers from Mount Waesche are known as the &quot;Great Wall&quot; and &quot;Yellow Wall&quot;. The volcano emerges through and is surrounded by the West Antarctic Ice Sheet. The ice sheet reaches an elevation of about above sea level at Mount Waesche and flows southward towards the Ross Ice Shelf. Blue ice is found in some areas.

Geographic entities mentioned:
surface_form: waesche
instance_of: Mountain
coordinates: lat: -77.166666666667
lon: -126.9
surface_form: mount waesche
instance_of: Mountain
coordinates: lat: -77.166666666667
lon: -126.9
Volcanic activity appears to be moving southward at a rate of. Seismic activity recorded in 2010 and 2011 south of Mount Waesche may indicate ongoing magmatic activity south of the youngest volcano. Chang Peak and Mount Waesche appear to be located outside of the Executive Committee Range volcanic lineament.

Geographic entities mentioned:
surface_form: waesche
instance_of: Mountain
coordinates: lat: -77.166666666667
lon: -126.9
surface_form: mount waesche
instance_of: Mountain
coordinates: lat: -77.166666666667
lon: -126.9
surface_form: mount waesche
instance_of: Mountain
coordinates: lat: -77.166666666667
lon: -126.9
Volcanic activity appears to be moving southward at a rate of. Seismic activity recorded in 2010 and 2011 south of Mount Waesche may indicate ongoing magmatic activity south of the youngest volcano. Chang Peak and Mount Waesche appear to be located outside of the Executive Committee Range volcanic lineament.

Geographic entities mentioned:
surface_form: waesche
instance_of: Mountain
coordinates: lat: -77.166666666667
lon: -126.9