Sarmila/GeoWiki-Features huggingface dataset:
This type of reserve is used for wildlife management or other specified wildlife purposes. The lake lies immediately to the south of the Hakatere Potts Road and is by road northwest of the small settlement of Mount Somers. There is a tramping and mountain biking track between Lake Camp and Lake Emma. There is a historic hut at Lake Emma with a tack shed and verandah.

Geographic entities mentioned:
surface_form: Lake Camp
instance_of: Lake
countries: New Zealand
coordinates: lat: -43.615
lon: 171.055
surface_form: lake camp
instance_of: Lake
countries: New Zealand
coordinates: lat: -43.615
lon: 171.055
surface_form: lake emma
instance_of: Lake
countries: New Zealand
coordinates: lat: -43.636
lon: 171.106
A case study report published by the Ministry for the Environment in 2023 reported that all the Ōtūwharekai/Ashburton Lakes were nutrient-enriched, with some at risk of deteriorating further into severe eutrophic states, changing from clear water with vegetation, to turbid algae-dominated water. The study reported that pastoral farming was the source for more than 90% of nutrients.

Geographic entities mentioned:
surface_form: ōtūwharekai
instance_of: Group of lakes
countries: New Zealand
coordinates: lat: -43.571666666666665
lon: 171.17555555555555
surface_form: ashburton lakes
instance_of: Group of lakes
countries: New Zealand
coordinates: lat: -43.572929
lon: 171.160126
Lake Emma (New Zealand). Lake Emma (), formerly known as Lake Acland'&quot;, is a high-country lake located in inland Canterbury in the South Island of New Zealand. The lake is shallow, with a maximum depth of and has a surface area of. The lake is popular for fishing.

Geographic entities mentioned:
surface_form: lake emma
instance_of: Lake
countries: New Zealand
coordinates: lat: -43.636
lon: 171.106
Lake Emma (New Zealand). Lake Emma (), formerly known as Lake Acland'&quot;, is a high-country lake located in inland Canterbury in the South Island of New Zealand. The lake is shallow, with a maximum depth of and has a surface area of. The lake is popular for fishing.

Geographic entities mentioned:
surface_form: lake acland
instance_of: Lake
countries: New Zealand
coordinates: lat: -43.636
lon: 171.106
surface_form: lake emma
instance_of: Lake
countries: New Zealand
coordinates: lat: -43.636
lon: 171.106
The lake is shallow, with a maximum depth of and has a surface area of. The lake is popular for fishing. The name Lake Emma was given by Thomas Potts in April 1957, who named the lake after his wife, during an exploration of the land between the upper Ashburton and Rakaia rivers. The lake was later named as Lake Acland. This name was gazetted in 1953, but was reverted to Lake Emma in 1969.

Geographic entities mentioned:
surface_form: lake acland
instance_of: Lake
countries: New Zealand
coordinates: lat: -43.636
lon: 171.106
The lake is shallow, with a maximum depth of and has a surface area of. The lake is popular for fishing. The name Lake Emma was given by Thomas Potts in April 1957, who named the lake after his wife, during an exploration of the land between the upper Ashburton and Rakaia rivers. The lake was later named as Lake Acland. This name was gazetted in 1953, but was reverted to Lake Emma in 1969.

Geographic entities mentioned:
surface_form: lake emma
instance_of: Lake
countries: New Zealand
coordinates: lat: -43.636
lon: 171.106
The lake is shallow, with a maximum depth of and has a surface area of. The lake is popular for fishing. The name Lake Emma was given by Thomas Potts in April 1957, who named the lake after his wife, during an exploration of the land between the upper Ashburton and Rakaia rivers. The lake was later named as Lake Acland. This name was gazetted in 1953, but was reverted to Lake Emma in 1969.

Geographic entities mentioned:
surface_form: lake emma
instance_of: Lake
countries: New Zealand
coordinates: lat: -43.636
lon: 171.106
surface_form: lake emma
instance_of: Lake
countries: New Zealand
coordinates: lat: -43.636
lon: 171.106
The lake lies immediately to the south of the Hakatere Potts Road and is by road northwest of the small settlement of Mount Somers. There is a tramping and mountain biking track between Lake Camp and Lake Emma. There is a historic hut at Lake Emma with a tack shed and verandah. It was constructed between the late 1860s and 1890, and was used as a musterer's hut.

Geographic entities mentioned:
surface_form: lake emma
instance_of: Lake
countries: New Zealand
coordinates: lat: -43.636
lon: 171.106
As the river runs its course through the city, it passes the city's original settlement location, Brisbane's Central Business District (CBD) at the curve of the river approximately upstream from Moreton Bay. The river is also artificially dammed by Wivenhoe Dam creating Lake Wivenhoe, which serves as the city's main water supply.

Geographic entities mentioned:
surface_form: Lake Wivenhoe
instance_of: Lake
countries: Australia
coordinates: lat: -27.25
lon: 152.51666666667
The D'Aguilar National Park, encompassing the D'Aguilar Range, bounds the north-west Brisbane's of built-up area, and contains the taller peaks of Mount Nebo, Camp Mountain, Mount Pleasant, Mount Glorious, Mount Samson and Mount Mee. Other prominent rises in Brisbane are Mount Gravatt and nearby Toohey Mountain.

Geographic entities mentioned:
surface_form: Mount Mee
instance_of: Mountain
countries: Australia
coordinates: lat: -27.074166666667
lon: 152.76972222222
The D'Aguilar National Park, encompassing the D'Aguilar Range, bounds the north-west Brisbane's of built-up area, and contains the taller peaks of Mount Nebo, Camp Mountain, Mount Pleasant, Mount Glorious, Mount Samson and Mount Mee. Other prominent rises in Brisbane are Mount Gravatt and nearby Toohey Mountain.

Geographic entities mentioned:
surface_form: Toohey Mountain
instance_of: Mountain
countries: Australia
coordinates: lat: -27.536713888889
lon: 153.03745
Other prominent rises in Brisbane are Mount Gravatt and nearby Toohey Mountain. Mount Petrie at and the lower rises of Highgate Hill, Mount Ommaney, Stephens Mountain, and Whites Hill are dotted across the city. Regions and parklands. Brisbane is part of the South-East Queensland region.

Geographic entities mentioned:
surface_form: Mount Petrie
instance_of: Mountain
countries: Australia
coordinates: lat: -27.533333333333
lon: 153.13333333333
The Glass House Mountains National Park is located to the north of the metropolitan area in the Glass House Mountains and provides green space between the Brisbane metropolitan area and the Sunshine Coast. The Tamborine National Park at Tamborine Mountain is located in the Gold Coast hinterland to the south of the metropolitan area.

Geographic entities mentioned:
surface_form: Tamborine Mountain
instance_of: Mountain
countries: Australia
coordinates: lat: -27.927513888889
lon: 153.19430555556
Hòn La bay is a 4-square-km marine bay with the depth up to 15 m and a surrounding land of 4 km2 suitable to develop sea deep-water port and industrial park. Mountains. The Hoành Sơn Mountains run through the northeastern part of the province. Many mount summits concentrate in Phong Nha-Kẻ Bàng area with over 1,000 metres height.

Geographic entities mentioned:
surface_form: Hoành Sơn Mountains
instance_of: Mountain
countries: Vietnam
coordinates: lat: 17.9911
lon: 106.3381
Quảng Bình province is the land of rich culture and famous people. There is an archaeological site of Bàu Tró, Phù Lưu ancient bronze drums in the time of Dong Son's culture. On 3 July 2007, an earthen pot of ancient coins weighing 20 kg was found buried at 500 cm underground in a paddy field and later sold for US$12.5 per kilo.

Geographic entities mentioned:
surface_form: Bàu Tró
instance_of: Lake
countries: Vietnam
coordinates: lat: 17.491388888889
lon: 106.62277777778
During his long artistic activities, Stanislav Hanzík organized dozens of exhibitions and created numerous important sculptures. These can be seen in places such as the Romanesque rotunda of St. George on the Říp Mountain, in the Czech National Theater, in front of Carolinum in the Old Town of Prague, and on the Old Steps of Prague Castle, etc.

Geographic entities mentioned:
surface_form: Říp
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.38653
lon: 14.2896344
1960: Welder (The Czech National Gallery, Prague; Gallery Litoměřice); 1964: Motherhood (nursery school, Most; the Czech National Gallery in Prague; Gallery Litoměřice); 1968: Mother Karyatida (monument for victims of Nazi concentration camp in Terezín); 1969: Impaled lion (crematorium of Most – devastated by vandals in 1990; The Czech National Gallery Prague); Dialog of a Poet and a Girl (sculptural open-air museum in Arandjelovac, Serbia)
1970: My Country (Most, atrium of the Czech bank); 1972: Josef Sudek, a bust (the Czech National Gallery in Prague; commemorative plaque in Prague); 1973: Chess Game (National Gallery in Prague); Lion's Fountain of Carolinum; 1974: Stanislav Neumann (foyer of the National Theatre, Prague); Courteous Dialogue (the castle park in Litvínov); 1976: the Good Shepherd (Rotunda of St.

Geographic entities mentioned:
surface_form: Říp
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.38653
lon: 14.2896344
Tirana. Tirana (,;) is the capital and largest city of Albania. It is located in the centre of the country, enclosed by mountains and hills, with Dajti rising to the east and a slight valley to the northwest overlooking the Adriatic Sea in the distance. It is among the wettest and sunniest cities in Europe, with 2,544 hours of sun per year.

Geographic entities mentioned:
surface_form: Dajti
instance_of: Mountain
countries: Albania
coordinates: lat: 41.365833333333
lon: 19.925555555556
Geography. Tirana extends at the Plain of Tirana in the centre of Albania between the mount of Dajti in the east, the hills of Kërrabe, Sauk and Vaqarr in the south, and a valley to the north overlooking the Adriatic Sea. The average altitude is about above sea level, with a maximum of at Maja Mincekut of Mali me Gropa in Shenmeri.

Geographic entities mentioned:
surface_form: Dajti
instance_of: Mountain
countries: Albania
coordinates: lat: 41.365833333333
lon: 19.925555555556
Despite the problems, the Grand Park at the Artificial Lake has some effect on absorbing CO2 emissions, while over 2.000 trees have been planted around sidewalks. Works for four new large parks have started in the summer of 2015 located in Kashar, Farkë, Vaqarr, and Dajt. These parks are part of the new urban plan striving to increase the concentration of green spaces in the capital.

Geographic entities mentioned:
surface_form: Farkë
instance_of: Lake
countries: Albania
coordinates: lat: 41.314722222222
lon: 19.860555555556
Bootleg footage from some of the concerts is interspersed with the professionally shot material. The front cover features West and East Mitten Buttes, photographed from the visitor centre at the Navajo Tribal Park located at Monument Valley, Arizona. Background and production. The reason for [the DVD] was that there was no visual material [of the band] that was out there really.

Geographic entities mentioned:
surface_form: West and East Mitten Buttes
instance_of: Mountain
countries: United States
coordinates: lat: 36.99
lon: -110.083
Cabrillo National Monument. Cabrillo National Monument () is a U.S. national monument at the southern tip of the Point Loma peninsula in San Diego, California. It commemorates the landing of Juan Rodríguez Cabrillo at San Diego Bay on September 28, 1542. This event marked the first time a European expedition had set foot on what later became the West Coast of the United States.

Geographic entities mentioned:
surface_form: Point Loma
instance_of: Landform
countries: United States
coordinates: lat: 32.67
lon: -117.24194444
Sacred Rock (Presque Isle County). Sacred Rock is an Engadine-dolomite boulder, now 20 feet long by 8 feet wide and 6 feet high, on the shore of Lake Huron in Northern Lower Michigan. It is located 6 miles north of Rogers City, Michigan, approximately 0.5 miles north of P.H. Hoeft State Park. Located in front of private cottages, the best way to reach the site is by turning east off of U.S.

Geographic entities mentioned:
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
The rock is located midway between the Ocqueoc River and Swan River, and served as a key boundary marker for competing tribes, as well as an altar for animal sacrifices. It was probably deposited by the last receding glaciers which formed the Great Lakes, and likely originated from the Lake Superior region of Canada.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
At last the chiefs of the two tribes met, when the one as usual was trespassing over the border, and an altercation ensued which would probably have again resulted in a bloody war between the conflicting tribes, but Kitchie Manitou, the Great Spirit, who was up Lake Superior at the time, became disgusted with both of them, seized hold of the Sacred Rock and hurled it down, crushing both the chiefs beneath its immense weight, which was so great, that the banks above the beach have been sliding and trembling ever since.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
Orlången Nature Reserve. Orlången Nature Reserve (&quot;Orlångens naturreservat&quot;) is a nature reserve surrounding Lake Orlången in central Huddinge Municipality, south of Stockholm, Sweden. Description. The reserve, founded in 1998, encompasses a total area of 15 square kilometres, of which 12 km² is land dominated by a system of rift valleys characteristic for South Stockholm.

Geographic entities mentioned:
surface_form: Orlången
instance_of: Lake
countries: Sweden
coordinates: lat: 59.197222222222
lon: 18.041666666667
The central part of the reserve is dominated by old agricultural lands and pastures, with preserved mansions and homesteads dating back to the 18th century. There are four lakes within the reserve: Trehörningen (Sjödalen), Ågestasjön, Orlången, and Mörtsjön.

Geographic entities mentioned:
surface_form: Ågestasjön
instance_of: Lake
countries: Sweden
coordinates: lat: 59.2225
lon: 18.074027777778
surface_form: Orlången
instance_of: Lake
countries: Sweden
coordinates: lat: 59.197222222222
lon: 18.041666666667
surface_form: Mörtsjön
instance_of: Lake
countries: Sweden
coordinates: lat: 59.214444444444
lon: 18.031111111111
There are four lakes within the reserve: Trehörningen (Sjödalen), Ågestasjön, Orlången, and Mörtsjön. Lake Ågestasjön in the north-eastern end of the reserve is one of the most important bird resting locales and breeding grounds in Stockholm County. Throughout the reserve there are a multitude of rare flora and fauna, making it important for regional biodiversity.

Geographic entities mentioned:
surface_form: Ågestasjön
instance_of: Lake
countries: Sweden
coordinates: lat: 59.2225
lon: 18.074027777778
According to G. Clauson, Old Turkic &quot;tul&quot; denotes &quot;widow, widower&quot;. Golden, citing Lajos Ligeti (1986), wondered if Dulo resulted from Slavicism of Turkic title Yula. Even so, all hypotheses P. B. Golden considers for now as speculative. Legacy. Dulo Hill on Livingston Island, near Antarctica, is named after the Bulgarian ruling dynasty Dulo.

Geographic entities mentioned:
surface_form: Dulo Hill
instance_of: Mountain
coordinates: lat: -62.5994
lon: -61.1578
The nearby states of India, such as Bihar, Uttar Pradesh and Assam, and parts of northern Bangladesh were also affected. The Kosi River filled to dangerous levels, while the Bagmati River and Nakkhu rivers caused flooding in Bagmati Province. The Kathmandu Valley received between and between 28 and 29 September, causing flooding in Nepal's capital, Kathmandu.

Geographic entities mentioned:
surface_form: Kathmandu Valley
instance_of: Valley
countries: Nepal
coordinates: lat: 27.703944444444
lon: 85.308583333333
Flooding in Nepal coincided with 2024 floods in neighbouring and nearby states of India, such as Uttar Pradesh and Assam. Nepalese weather official Binu Maharjan stated that a low-pressure system lingering over nearby regions of India and over the Bay of Bengal was the primary cause of the increased and prolonged flooding in 2024.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
Bagmati Province was heavily impacted by the flooding of the Bagmati River and the Nakkhu River. Kathmandu Valley received between and of rain over a period of 24 hours from the mornings of 28–29 September, representing the capital's largest recorded rainfall since 1970 at the latest. As of October 1 at least 217 deaths and 28 missing were confirmed due to flooding.

Geographic entities mentioned:
surface_form: Kathmandu Valley
instance_of: Valley
countries: Nepal
coordinates: lat: 27.703944444444
lon: 85.308583333333
Much of the city also lost power and internet, and multiple water pipes were broken. Thousands of residents were displaced. At least 37 people were killed in the city, and 56 total deaths were reported in the wider Kathmandu Valley. Across Nepal, at least 322 houses and 16 bridges were damaged. Nepalese media described the rainfall as the worst that Kathmandu had suffered from in decades.

Geographic entities mentioned:
surface_form: Kathmandu Valley
instance_of: Valley
countries: Nepal
coordinates: lat: 27.703944444444
lon: 85.308583333333
Several miles beyond, US 209 crosses into Carbon County at Lansford, where it nestles between Nesquehoning, Sharp, and Pisgah mountains until it finally turns slightly to the north just before Nesquehoning. From there it follows the Nesquehoning Creek valley down to the Lehigh River, which US 209 follows southeasterly through Jim Thorpe to Lehighton.

Geographic entities mentioned:
surface_form: Nesquehoning
instance_of: Landform
countries: United States
coordinates: lat: 40.8333
lon: -75.9158
surface_form: Sharp
instance_of: Mountain
countries: United States
coordinates: lat: 40.86182
lon: -75.83966
Mount Senger is a mountain summit located west of the crest of the Sierra Nevada mountain range in Fresno County of northern California, United States. It is set within the John Muir Wilderness, on land managed by Sierra National Forest. It is situated southeast of Mount Hooper, southwest of Gemini, and south-southwest of Seven Gables. Senger ranks as the 348th-highest summit in California.

Geographic entities mentioned:
surface_form: Mount Hooper
instance_of: Mountain
countries: Australia
coordinates: lat: -12.2896
lon: 132.3657
surface_form: Seven Gables
instance_of: Mountain
countries: United States
coordinates: lat: 37.311388888889
lon: -118.83361111111
surface_form: gemini
instance_of: Mountain
countries: United States
coordinates: lat: 37.296944444444
lon: -118.81638888889
Mount Senger. Mount Senger is a mountain summit located west of the crest of the Sierra Nevada mountain range in Fresno County of northern California, United States. It is set within the John Muir Wilderness, on land managed by Sierra National Forest. It is situated southeast of Mount Hooper, southwest of Gemini, and south-southwest of Seven Gables.

Geographic entities mentioned:
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: mount senger
instance_of: Mountain
countries: United States
coordinates: lat: 37.277777777778
lon: -118.85861111111
Mount Senger. Mount Senger is a mountain summit located west of the crest of the Sierra Nevada mountain range in Fresno County of northern California, United States. It is set within the John Muir Wilderness, on land managed by Sierra National Forest. It is situated southeast of Mount Hooper, southwest of Gemini, and south-southwest of Seven Gables.

Geographic entities mentioned:
surface_form: mount senger
instance_of: Mountain
countries: United States
coordinates: lat: 37.277777777778
lon: -118.85861111111
Davis, T. G. Gerdine, C. F. Urquhart, and L. F. Biggs. Today this peak draws climbing interest because it is included on the Sierra Peaks Section's peak bagging list. Climate. According to the Köppen climate classification system, Mount Senger is located in an alpine climate zone. Most weather fronts originate in the Pacific Ocean, and travel east toward the Sierra Nevada mountains.

Geographic entities mentioned:
surface_form: mount senger
instance_of: Mountain
countries: United States
coordinates: lat: 37.277777777778
lon: -118.85861111111
The specific epithet (&quot;squarrosa&quot;) means &quot;thickly crowded and rigid&quot;, referring to the leaves. Distribution. This species of pea grows in forest, mainly in near-coastal areas, from south-east Queensland to the Tuross River in New South Wales, but also as far inland as the Megalong Valley and Goulburn.

Geographic entities mentioned:
surface_form: Megalong Valley
instance_of: Valley
countries: Australia
coordinates: lat: -33.733333333333
lon: 150.25
In 1941 he joined the Italian army as an officer. After September 8, 1943, he sought refuge in Switzerland (where he met European intellectuals, politicians and critics), then in 1944 he returned to fight with the partisans in Valdossola. When the war was over he settled in Milan, working as journalist, copywriter and translator.

Geographic entities mentioned:
surface_form: Valdossola
instance_of: Valley
countries: Italy
coordinates: lat: 46.283333333333
lon: 8.35
Jefferson County, West Virginia. Jefferson County is the easternmost county in the U.S. state of West Virginia. It is located in the Shenandoah Valley in the Eastern Panhandle of West Virginia. As of the 2020 census, the population was 57,701. Its county seat is Charles Town. The county was founded in 1801, and today is part of the Washington metropolitan area. Formation.

Geographic entities mentioned:
surface_form: Shenandoah Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.5
lon: -78.85
Joining West Virginia. Jefferson County had voted for secession in the vote taken on May 23, 1861. However, Jefferson County, along with Berkeley County, both counties lying on the Potomac River in the Shenandoah Valley, with the consent of the Reorganized Government of Virginia voted in favor of annexation to West Virginia in 1863.

Geographic entities mentioned:
surface_form: Shenandoah Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.5
lon: -78.85
History. The initial formation of the Facho-Pico Alto Volcanic Complex was a phase of intense volcanism, resulting from submarine eruptions as early as 5 million years ago, resulting in the formation of Pico do Facho and extensive pillow lavas. Remnants of these pillow lavas can be identified above sea level, helping to increase the size of the island to roughly its current dimensions.

Geographic entities mentioned:
surface_form: pico do facho
instance_of: Mountain
countries: Portugal
coordinates: lat: 33.0852
lon: -16.3249
surface_form: pico
instance_of: Mountain
countries: Portugal
coordinates: lat: 38.468611111111
lon: -28.399166666667
surface_form: pico
instance_of: Mountain
countries: Portugal
coordinates: lat: 38.468611111111
lon: -28.399166666667
surface_form: pico alto
instance_of: Mountain
countries: Portugal
coordinates: lat: 36.98326111
lon: -25.09060278
The volcanism that originated Facho was submarine in nature, with two visible centres positioned in the southern part of the island: Pico do Facho and a second pyroclastic cone situated west of Rocha Alta (the remains of its chamber still visible along the coast). Both these emission centre were responsible for pyroclastic and submarine lava flows.

Geographic entities mentioned:
surface_form: pico do facho
instance_of: Mountain
countries: Portugal
coordinates: lat: 33.0852
lon: -16.3249
surface_form: pico
instance_of: Mountain
countries: Portugal
coordinates: lat: 38.468611111111
lon: -28.399166666667
Pico Alto (Santa Maria). Pico Alto (literally &quot;high/tall peak&quot;) is a mountain which is the highest point, on the island of Santa Maria, in the Portuguese archipelago of the Azores. History.

Geographic entities mentioned:
surface_form: pico
instance_of: Mountain
countries: Portugal
coordinates: lat: 38.468611111111
lon: -28.399166666667
surface_form: pico alto (santa maria)
instance_of: Mountain
countries: Portugal
coordinates: lat: 36.98326111
lon: -25.09060278
Pico Alto (Santa Maria). Pico Alto (literally &quot;high/tall peak&quot;) is a mountain which is the highest point, on the island of Santa Maria, in the Portuguese archipelago of the Azores. History.

Geographic entities mentioned:
surface_form: pico
instance_of: Mountain
countries: Portugal
coordinates: lat: 38.468611111111
lon: -28.399166666667
surface_form: pico alto
instance_of: Mountain
countries: Portugal
coordinates: lat: 36.98326111
lon: -25.09060278
The Pico Alto complex occurred continuously between 5 and 3 million years ago. On 8 February 1989 Independent Air Flight 1851 struck Pico Alto due to pilot error killing all 144 on board in the worst air crash in Portuguese history.

Geographic entities mentioned:
surface_form: pico
instance_of: Mountain
countries: Portugal
coordinates: lat: 38.468611111111
lon: -28.399166666667
surface_form: pico alto
instance_of: Mountain
countries: Portugal
coordinates: lat: 36.98326111
lon: -25.09060278
On 5 December 2012, the &quot;Secretaria Regional dos Recursos Naturais&quot; (&quot;Regional Directorate for Natural Resources&quot;) announced that they were beginning a reforestation program for Pico Alto; the forest of Santa Maria was considered &quot;more identitical to those original [pre-colonization] forests of the Azores&quot;.

Geographic entities mentioned:
surface_form: pico
instance_of: Mountain
countries: Portugal
coordinates: lat: 38.468611111111
lon: -28.399166666667
surface_form: pico alto
instance_of: Mountain
countries: Portugal
coordinates: lat: 36.98326111
lon: -25.09060278
Geography. The island of Santa Maria was created from successive layers of volcanic materials and marine sediments stratified over the course of a formative period, of which Pico Alto was created between 2 and 5 million years ago.

Geographic entities mentioned:
surface_form: pico
instance_of: Mountain
countries: Portugal
coordinates: lat: 38.468611111111
lon: -28.399166666667
surface_form: pico alto
instance_of: Mountain
countries: Portugal
coordinates: lat: 36.98326111
lon: -25.09060278
The oldest island in the Azores, many of the original geological structures and volcanic morphology has been totally or partially eroded, dismantled and difficult to detect in the landscape of the island. Pico Alto being the largest structure within the &quot;Facho-Pico Alto Volcanic Complex&quot; has persisted throughout the island's geological history.

Geographic entities mentioned:
surface_form: pico
instance_of: Mountain
countries: Portugal
coordinates: lat: 38.468611111111
lon: -28.399166666667
surface_form: pico alto
instance_of: Mountain
countries: Portugal
coordinates: lat: 36.98326111
lon: -25.09060278
Geomorphologically, Pico Alto is part of a sierra localized in the central part of the island, consisting of a mountainous north–south alignment dividing the a rugged eastern coast from the western plain that rarely exceeds in elevation. The eastern or mountainous zone, is covered almost completely in vegetation, and highlighted by the peaks of Pico Alto, Cavacas, and Caldeiras.

Geographic entities mentioned:
surface_form: pico
instance_of: Mountain
countries: Portugal
coordinates: lat: 38.468611111111
lon: -28.399166666667
surface_form: pico
instance_of: Mountain
countries: Portugal
coordinates: lat: 38.468611111111
lon: -28.399166666667
surface_form: pico alto
instance_of: Mountain
countries: Portugal
coordinates: lat: 36.98326111
lon: -25.09060278
surface_form: pico alto
instance_of: Mountain
countries: Portugal
coordinates: lat: 36.98326111
lon: -25.09060278
The eastern or mountainous zone, is covered almost completely in vegetation, and highlighted by the peaks of Pico Alto, Cavacas, and Caldeiras. The Facho-Pico Alto Volcanic Complex was constructed in three phases: the first related to stratovolcanic unit of Facho, and then, two lateral centres associated with Pico Alto.

Geographic entities mentioned:
surface_form: pico
instance_of: Mountain
countries: Portugal
coordinates: lat: 38.468611111111
lon: -28.399166666667
surface_form: pico alto
instance_of: Mountain
countries: Portugal
coordinates: lat: 36.98326111
lon: -25.09060278
The periods of sub-aerial activity resulted in extensive outcroppings, lava fields, layered pyroclasts, dykes and numerous seams (approximately 230), that originated in the central relief of Cavacas until Caldeira, and passing through Pico Alto, while submarine lava flows extended into the sea in the Bay of São Lourenço, Maia and Ponta do Castelo.

Geographic entities mentioned:
surface_form: pico
instance_of: Mountain
countries: Portugal
coordinates: lat: 38.468611111111
lon: -28.399166666667
surface_form: pico alto
instance_of: Mountain
countries: Portugal
coordinates: lat: 36.98326111
lon: -25.09060278
He is the son of captain Bergvin Oddsson and María Friðriksdóttir. He and his family moved to Vestmannaeyjar when he was a few months old. Other than the a year he spent in Grindavík following the 1973 eruption of the Eldfell volcano, he spent most of his childhood in Vestmannaeyjar. He received a master's license for operating a 30-tonne vessel in 1980.

Geographic entities mentioned:
surface_form: Eldfell
instance_of: Mountain
countries: Iceland
coordinates: lat: 63.4333008635
lon: -20.2487692886
There are only 20 ancient lakes over 1 million years old. Lake Baikal is often considered the oldest, as clear evidence shows that it is 25–30 million years old. Lake Zaysan may be even older, of Cretaceous origin and at least 66 million years old (most likely around 70 million years), but its exact age is controversial and labeled with some uncertainty.

Geographic entities mentioned:
surface_form: Lake Baikal
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.30277778
lon: 108.00472222
Lake Baikal is often considered the oldest, as clear evidence shows that it is 25–30 million years old. Lake Zaysan may be even older, of Cretaceous origin and at least 66 million years old (most likely around 70 million years), but its exact age is controversial and labeled with some uncertainty. Another contender for oldest is Lake Maracaibo, estimated to be 20–36 million years old.

Geographic entities mentioned:
surface_form: Lake Zaysan
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 48
lon: 84
Lake Baikal is often considered the oldest, as clear evidence shows that it is 25–30 million years old. Lake Zaysan may be even older, of Cretaceous origin and at least 66 million years old (most likely around 70 million years), but its exact age is controversial and labeled with some uncertainty. Another contender for oldest is Lake Maracaibo, estimated to be 20–36 million years old.

Geographic entities mentioned:
surface_form: Lake Maracaibo
instance_of: Lake
countries: Venezuela
coordinates: lat: 9.8158333333333
lon: -71.556666666667
Ancient lakes have a prolonged life when compared to younger, more ordinary lakes due to the local active rift zones and subsided sections of land called grabens. For example, Lake Baikal in Russia, the deepest lake in the world, is an ancient lake created by the Baikal Rift Zone which is 25–30 million years old and deep.

Geographic entities mentioned:
surface_form: Lake Baikal
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.30277778
lon: 108.00472222
Evolutionary characteristics including sexual selection, adaptive radiation and punctuated equilibrium are studied in ancient lakes due to their prolonged existence and general geographic isolation. Most of the research has been associated with the endemic fauna and diatoms that exist in these isolated lakes, concentrating on Lake Baikal, the Caspian Sea and the African Great Lakes.

Geographic entities mentioned:
surface_form: Lake Baikal
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.30277778
lon: 108.00472222
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
surface_form: African Great Lakes
instance_of: Group of lakes
countries: Burundi
Zambia
Kenya
Democratic Republic of the Congo
Malawi
Mozambique
Rwanda
Tanzania
Uganda
Ethiopia
coordinates: lat: -8
lon: 35
Demon (volcano). Demon (;;) is a stratovolcano located at the northern end of Iturup Island, in the Kuril Archipelago. The Ilya Muromets Waterfall (Rakkibetsu Waterfall) falls abruptly from the eastern slope of the volcano into the Pacific Ocean.

Geographic entities mentioned:
surface_form: demon
instance_of: Mountain
countries: Russia
Soviet Union
Empire of Japan
Russian Empire
Japan
coordinates: lat: 45.5014
lon: 148.8603
Vulsini. Vulsini, also known as Volsini volcano, Vulsini Volcanic District, Vulsini Volcanic Complex and the Vulsinian District, is a circular region of intrusive igneous rock in Lazio, Italy, about to the north northwest of Rome, containing a cluster of calderas known to have been active in recent geologic times.

Geographic entities mentioned:
surface_form: vulsini
instance_of: Mountain
countries: Italy
coordinates: lat: 42.6
lon: 11.933333333333
Vulsini. Vulsini, also known as Volsini volcano, Vulsini Volcanic District, Vulsini Volcanic Complex and the Vulsinian District, is a circular region of intrusive igneous rock in Lazio, Italy, about to the north northwest of Rome, containing a cluster of calderas known to have been active in recent geologic times.

Geographic entities mentioned:
surface_form: vulsini
instance_of: Mountain
countries: Italy
coordinates: lat: 42.6
lon: 11.933333333333
surface_form: vulsini
instance_of: Mountain
countries: Italy
coordinates: lat: 42.6
lon: 11.933333333333
surface_form: vulsini
instance_of: Mountain
countries: Italy
coordinates: lat: 42.6
lon: 11.933333333333
The Volsinian is the northernmost region. At relatively low altitude, the Vulsini calderas cover about and contain four Pleistocene-age depressions known as Bolsena, Latera, Vepe and Montefiascone calderas. An alleged eruption occurred in 104 BC, but it is currently considered a misinterpretation of the description of a fire, and the most recent confirmed activity occurred in Pleistocene.

Geographic entities mentioned:
surface_form: vulsini
instance_of: Mountain
countries: Italy
coordinates: lat: 42.6
lon: 11.933333333333
In addition the small Montefiascone caldera, also nested, lies between Montefiascone on its eastern rim and the lake. Two islands in the lake, Bisentina and Martana, were formed from airfall tuffs in Pompeii-like eruptions. Dozens of other tuff cones dot the region, mainly on the eastern side of the complex. The Italian Civil Protection Department considers Vulsini as extinct.

Geographic entities mentioned:
surface_form: vulsini
instance_of: Mountain
countries: Italy
coordinates: lat: 42.6
lon: 11.933333333333
Army at Camp A.E. Wood in the Wawona district of the park in 1904 to house the commander of the military administration that operated the park in the years prior to the establishment of the National Park Service. It was moved to the Yosemite Valley in 1906. The Acting Superintendent's Headquarters is the last remaining structure at Wawona associated with the park's military administration.

Geographic entities mentioned:
surface_form: Yosemite Valley
instance_of: Valley
countries: United States
coordinates: lat: 37.721694444444445
lon: -119.646
Nipissis River. The Nipissis River (,) is a river in the Côte-Nord region of Quebec, Canada, a tributary of the Moisie River. It is a recognized salmon river. The river is known for its steep cliffs, which provide a challenging ice-climbing environment. Location. The Nipissis River is in the unorganized territory of Rivière-Nipissis in the Sept-Rivières Regional County Municipality.

Geographic entities mentioned:
surface_form: Moisie River
instance_of: Watercourse
countries: Canada
coordinates: lat: 50.2
lon: -66.0675
Tributaries include the Wacouno and Nipisso rivers, both of which enter from the left. The Nipissis drains a region of, making it the most important tributary of the Moise River. It is followed by the Aux Pékans River, which drains an area of. The proposed Moisie River Aquatic Reserve would include the Nipissis River and a narrow strip along its shores. The Nipissis River is a little over long.

Geographic entities mentioned:
surface_form: Aux Pékans River
instance_of: Watercourse
countries: Canada
coordinates: lat: 52.20638888888889
lon: -66.81055555555555
The Wacouno River joins the Nipissis to the west of Lake Nipisso. It runs south from the Lake Fournier region. The Nipisso River, from Lake Nipisso, joins the Nipissis about above its confluence with the Moisie. The McDonald River joins the Nipissis not far from its mouth at the Chute McDonald, or McDonald Falls. Name.

Geographic entities mentioned:
surface_form: Lake Nipisso
instance_of: Lake
countries: Canada
coordinates: lat: 50.85667
lon: -65.82417
Location. This mountainous territory is located to the south of the Diois region, the Drôme river and the natural and historical region of Dauphiné. It is surrounded by the Vercors massif to the north of the Drôme, the Dévoluy massif and the Bochaine mountains to the east of Buëch and the Baronnies massif to the south of Aigues. Geology.

Geographic entities mentioned:
surface_form: Bochaine mountains
instance_of: Valley
countries: France
Orkland Municipality. Orkland is a municipality in Trøndelag county, Norway. It is located in the traditional district of Orkdalen. The administrative centre of the municipality is the town of Orkanger.

Geographic entities mentioned:
surface_form: Orkdalen
instance_of: Valley
countries: Norway
coordinates: lat: 63.233333333333
lon: 9.7666666666667
General information. Orkland Municipality was established on 1 January 2020 after a large municipal merger which combined Agdenes Municipality, Orkdal Municipality, Meldal Municipality, and most of Snillfjord Municipality. Name. The municipality is named after the Orkdalen valley (). The first element is the genitive case of the name of the river (now called Orklaelva).

Geographic entities mentioned:
surface_form: Orkdalen
instance_of: Valley
countries: Norway
coordinates: lat: 63.233333333333
lon: 9.7666666666667
Geography. The municipality encompasses a lot of the Orkdalen valley, plus coastal areas along the Trondheimsfjorden and Trondheimsleia. Hitra Municipality, Heim Municipality, and Rindal Municipality are located to the west, Rennebu Municipality is to the south, and Midtre Gauldal Municipality, Melhus Municipality, and Skaun Municipality are located to the east.

Geographic entities mentioned:
surface_form: Orkdalen
instance_of: Valley
countries: Norway
coordinates: lat: 63.233333333333
lon: 9.7666666666667
It also includes Calton Hill, the shops and offices on the northern side of Princes Street, Bute House, the official residence of the First Minister of Scotland, St Mary's Episcopal Cathedral, the Edinburgh Playhouse, the Edinburgh Waterfront, the stretch of the Water of Leith from Dean Village to Leith Harbour, the Royal Botanical Gardens, the Western General Hospital and the notable private schools.

Geographic entities mentioned:
surface_form: Calton Hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 55.955278
lon: -3.182222
Schwabenkopf. The Schwabenkopf is a mountain in the Kaunergrat group of the Ötztal Alps.

Geographic entities mentioned:
surface_form: ötztal
instance_of: Valley
countries: Austria
coordinates: lat: 47.136944
lon: 10.927222
surface_form: schwabenkopf
instance_of: Mountain
countries: Austria
coordinates: lat: 47.006388888889
lon: 10.793888888889
Schwabenkopf. The Schwabenkopf is a mountain in the Kaunergrat group of the Ötztal Alps.

Geographic entities mentioned:
surface_form: schwabenkopf
instance_of: Mountain
countries: Austria
coordinates: lat: 47.006388888889
lon: 10.793888888889
Staten Island Heights. Staten Island Heights () is a predominantly flat, ice-covered upland between Greenville Valley and Alatna Valley in the Convoy Range of Victoria Land, Antarctica. Exploration and naming. Staten Island Heights were mapped by the United States Geological Survey (USGS) from ground surveys and Navy air photos.

Geographic entities mentioned:
surface_form: Alatna Valley
instance_of: Valley
coordinates: lat: -76.883333333333
lon: 161.16666666667
One of the nautical names in Convoy Range. So named by a NZARP field party in the 1989-90 season. Pascoe Glacier. A cirque glacier, long, which flows into Greenville Valley from the north end of Staten Island Heights. The name was applied by geologist Christopher J. Burgess, VUWAE party leader in the 1976-77 season. Named after John D.

Geographic entities mentioned:
surface_form: Greenville Valley
instance_of: Valley
coordinates: lat: -76.7333
lon: 160.867
Lar National Park (Persian پارک ملی لار &quot;park-e melli-e lar&quot;) is a protected area in Amol County of Mazandaran Province in northern Iran. Geography. The park is in the Central Alborz mountain range, at the foot of Mount Damavand. It has been a national park since 1976 and a protected area since 1982 by the Iran Department of Environment. Since 1991 hunting has been prohibited.

Geographic entities mentioned:
surface_form: Mount Damavand
instance_of: Mountain
countries: Iran
coordinates: lat: 35.955277777778
lon: 52.109166666667
&quot;Betula pubescens&quot; has a wide distribution in northern and central Europe and Asia. Its range extends from Newfoundland, Iceland, the British Isles and Spain eastwards across northern and central Europe and Asia as far as the Lake Baikal region in Siberia. The range extends southwards to about 40°N, its southernmost limit being Turkey, the Caucasus and the Altai Mountains.

Geographic entities mentioned:
surface_form: Lake Baikal
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.30277778
lon: 108.00472222
The fruit is a capsule about long containing winged seeds. Taxonomy. &quot;Pandorea nervosa&quot; was first formally described in 1931 by Cornelis Gijsbert Gerrit Jan van Steenis in the Journal of the Arnold Arboretum from specimens collected near Boonjie on the Atherton Tableland in 1929. The specific epithet (&quot;nervosa&quot;) means &quot;many veins&quot;. Distribution and habitat.

Geographic entities mentioned:
surface_form: Atherton Tableland
instance_of: Plateau
countries: Australia
coordinates: lat: -17.16666667
lon: 145.53333333
Almost immediately after publication, the book was proven to be completely fictitious. Seltzer was revealed to have grown up with her two white biological parents in the San Fernando Valley community of Sherman Oaks. She had also attended Campbell Hall, an Episcopalian day school in the North Hollywood area of Los Angeles.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
Pyhäjärvi (Saarijärvi). Pyhäjärvi (Saarijärvi) is a medium-sized lake of Central Finland, located in the northern side of Saarijärvi municipality's center. It belongs to Kymijoki mean catchment area. Pyhäjärvi (meaning: Holy lake) is very common name in Finland. There are 39 lakes with the same name.

Geographic entities mentioned:
surface_form: pyhäjärvi
instance_of: Lake
countries: Finland
coordinates: lat: 61.48333333
lon: 23.66666667
surface_form: pyhäjärvi
instance_of: Lake
countries: Finland
coordinates: lat: 60.9889329
lon: 22.2989207
surface_form: saarijärvi
instance_of: Lake
countries: Finland
coordinates: lat: 65.283333333333
lon: 28.383333333333
surface_form: saarijärvi
instance_of: Lake
countries: Finland
coordinates: lat: 62.7
lon: 25.2167
surface_form: pyhäjärvi (saarijärvi)
instance_of: Lake
countries: Finland
coordinates: lat: 62.7238
lon: 25.46206
surface_form: pyhäjärvi
instance_of: Lake
countries: Finland
coordinates: lat: 63.58333333
lon: 25.95
surface_form: pyhäjärvi
instance_of: Lake
countries: Finland
coordinates: lat: 61.013333
lon: 26.491667
Pyhäjärvi (Saarijärvi). Pyhäjärvi (Saarijärvi) is a medium-sized lake of Central Finland, located in the northern side of Saarijärvi municipality's center. It belongs to Kymijoki mean catchment area. Pyhäjärvi (meaning: Holy lake) is very common name in Finland. There are 39 lakes with the same name.

Geographic entities mentioned:
surface_form: pyhäjärvi
instance_of: Lake
countries: Finland
coordinates: lat: 61.48333333
lon: 23.66666667
surface_form: pyhäjärvi
instance_of: Lake
countries: Finland
coordinates: lat: 60.9889329
lon: 22.2989207
surface_form: saarijärvi
instance_of: Lake
countries: Finland
coordinates: lat: 65.283333333333
lon: 28.383333333333
surface_form: saarijärvi
instance_of: Lake
countries: Finland
coordinates: lat: 65.283333333333
lon: 28.383333333333
surface_form: saarijärvi
instance_of: Lake
countries: Finland
coordinates: lat: 62.7
lon: 25.2167
surface_form: saarijärvi
instance_of: Lake
countries: Finland
coordinates: lat: 62.7
lon: 25.2167
surface_form: pyhäjärvi (saarijärvi)
instance_of: Lake
countries: Finland
coordinates: lat: 62.7238
lon: 25.46206
surface_form: pyhäjärvi
instance_of: Lake
countries: Finland
coordinates: lat: 63.58333333
lon: 25.95
surface_form: pyhäjärvi
instance_of: Lake
countries: Finland
coordinates: lat: 61.013333
lon: 26.491667
Pyhäjärvi (Saarijärvi). Pyhäjärvi (Saarijärvi) is a medium-sized lake of Central Finland, located in the northern side of Saarijärvi municipality's center. It belongs to Kymijoki mean catchment area. Pyhäjärvi (meaning: Holy lake) is very common name in Finland. There are 39 lakes with the same name.

Geographic entities mentioned:
surface_form: pyhäjärvi
instance_of: Lake
countries: Finland
coordinates: lat: 61.48333333
lon: 23.66666667
surface_form: pyhäjärvi
instance_of: Lake
countries: Finland
coordinates: lat: 60.9889329
lon: 22.2989207
surface_form: pyhäjärvi
instance_of: Lake
countries: Finland
coordinates: lat: 62.7238
lon: 25.46206
surface_form: pyhäjärvi
instance_of: Lake
countries: Finland
coordinates: lat: 63.58333333
lon: 25.95
surface_form: pyhäjärvi
instance_of: Lake
countries: Finland
coordinates: lat: 61.013333
lon: 26.491667
Gasherbrum is often claimed to mean &quot;Shining Wall&quot;, presumably a reference to the highly visible face of Gasherbrum IV; but in fact it comes from &quot;rgasha&quot; (beautiful) + &quot;brum&quot; (mountain) in Balti, hence it actually means &quot;beautiful mountain.&quot;
While the four highest Gasherbrum peaks (Gasherbrum I to IV) have been named and numbered since the 19th century, Gasherbrum V (as well as its neighbour Gasherbrum VI) were only considered as &quot;Peaks on the south ridge of Gasherbrum IV&quot;.

Geographic entities mentioned:
surface_form: Gasherbrum VI
instance_of: Mountain
countries: Pakistan
coordinates: lat: 35.708333333333
lon: 76.630833333333
surface_form: gasherbrum v
instance_of: Mountain
countries: Pakistan
coordinates: lat: 35.729722222222
lon: 76.6125
surface_form: gasherbrum vi
instance_of: Mountain
countries: Pakistan
coordinates: lat: 35.708333333333
lon: 76.630833333333
Gasherbrum V. Gasherbrum V () is a mountain in the Gasherbrum massif, located in the Karakoram range in Gilgit–Baltistan, Pakistan. Location and naming. The Gasherbrum massif is a remote group of peaks located at the northeastern end of the Baltoro Glacier in the Karakoram range of the Himalaya. The massif contains three of the world's 8,000 metre peaks (if one includes Broad Peak).

Geographic entities mentioned:
surface_form: gasherbrum v
instance_of: Mountain
countries: Pakistan
coordinates: lat: 35.729722222222
lon: 76.6125
The Swiss geologist and Himalayan expert Günter Oskar Dyhrenfurth recommended to give this independent mountain an own name and proposed in 1934 the name of &quot;Gasherbrum V&quot;, which is now well established. Altitude and climbing status. Although in former literature a height around 7,320 m was traditionally given, the mountain is more likely to be around 7,150 m high.

Geographic entities mentioned:
surface_form: gasherbrum v
instance_of: Mountain
countries: Pakistan
coordinates: lat: 35.729722222222
lon: 76.6125