Sarmila/GeoWiki-Features huggingface dataset:
Their journey was the first open boat transit from West to East and covered around 3,000 miles (2,600 nautical miles or 4,800 km), taking a route through Dolphin and Union Strait following the south coast of Victoria Island and King William Island, north to Resolute Bay via the Franklin Strait and Peel Sound, around the south and east coasts of Devon Island, through Hell Gate and across Norwegian Bay to Eureka, Greely Bay and the head of Tanquary Fiord.

Geographic entities mentioned:
surface_form: Peel Sound
instance_of: Watercourse
countries: Canada
coordinates: lat: 73
lon: -96.5
Once they reached Tanquary Fiord, they had to trek a further 150 miles via Lake Hazen to Alert before setting up their winter base camp. In 1992 Fiennes led an expedition that discovered what may be an outpost of the lost city of Iram in Oman. The following year he joined nutrition specialist Mike Stroud to become the first to cross the Antarctic continent unsupported; they took 93 days.

Geographic entities mentioned:
surface_form: Lake Hazen
instance_of: Lake
countries: Canada
coordinates: lat: 81.79722222222222
lon: -71.01666666666667
Fiennes later said that he forgot to pack his heart-rate monitor, and therefore did not know how fast his heart was beating. In June 2005, Fiennes had to abandon an attempt to be the oldest Briton to climb Mount Everest when, in another climb for charity, he was forced to turn back as a result of heart problems, after reaching the final stopping point of the ascent.

Geographic entities mentioned:
surface_form: Mount Everest
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.988055555555555
lon: 86.925
In March 2007, despite a lifelong fear of heights, Fiennes climbed the Eiger by its North Face, with sponsorship totalling £1.8 million to be paid to the Marie Curie Cancer Care Delivering Choice Programme. Kenton Cool first met Fiennes in 2004, and subsequently guided him in the Alps and Himalayas.

Geographic entities mentioned:
surface_form: Eiger
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.577607529
lon: 8.005286822
Coedydd Maentwrog National Nature Reserve. Coedydd Maentwrog, on the north side of the Vale of Ffestiniog, is the largest wood in the Vale (which runs from the coast at Porthmadog inland to Blaenau Ffestiniog in Gwynedd). The national nature reserve consists of two separate sections: Coed Llyn Mair, and a group of three forests (Coed Ty Coch, Coed Bronturnor and Coed Glanrafon).

Geographic entities mentioned:
surface_form: Vale of Ffestiniog
instance_of: Valley
countries: United Kingdom
coordinates: lat: 52.944
lon: -4.006
The national nature reserve consists of two separate sections: Coed Llyn Mair, and a group of three forests (Coed Ty Coch, Coed Bronturnor and Coed Glanrafon). It offers a variety of habitats, rising from the wooded valley onto open moorland and reaching towards the foot of Moelwyn Bach mountain.

Geographic entities mentioned:
surface_form: Moelwyn Bach
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.97385
lon: -3.9970111111111
Nebraska. After Brigham Young and the church were forced to leave Nauvoo in 1846, Stout served as the chief of police in Winter Quarters, Nebraska, when the Latter Day Saints migrated there. An early Mormon pioneer, Stout arrived in the Salt Lake Valley as a member of Heber C. Kimball's company in September 1848.

Geographic entities mentioned:
surface_form: Salt Lake Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.6839
lon: -111.978
Personal life. He was born in the small County Londonderry townland of Ballymaguigan in Northern Ireland, on the western shores of Lough Neagh in 1947 or 1948. His son Gary, was also a talented footballer and was left half back on the victorious 1993 Derry team; also winning an All Star for his performances that year. Inter-county.

Geographic entities mentioned:
surface_form: Lough Neagh
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.618333333333
lon: -6.3952777777778
She has trained and led multi-national teams of men and women on more than 50 expeditions to over 20 countries to include the Arctic and Antarctica. Jules has climbed 19 high-altitude mountains, reaching a personal best height of 7000m on Cho Oyu in Tibet. Lewis 2003, Jules has facilitated expeditions to raise awareness and funds for breast cancer in the United Arab Emirates.

Geographic entities mentioned:
surface_form: Cho Oyu
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 28.094166666667
lon: 86.660833333333
At Wardour it is joined by the River Sem. The river then flows east through Tisbury, where it is joined by the Fonthill Brook, and then onto Barford St Martin and Burcombe before reaching Wilton. Near Quidhampton, the Wylye joins from the north. After passing Harnham, the Nadder joins the Avon near Salisbury Cathedral. Including its headwaters, the river's length is about. Water quality.

Geographic entities mentioned:
surface_form: Fonthill Brook
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.086380555556
lon: -2.0970388888889
Other notable buildings include projects with her partner Davis such as Joseph Phelps Vineyards, Rutherford Hill Winery, Sullivan Vineyards, all in Sonoma Valley and Napa Valley California, the Caletti Jungsten building (1986) in Mill Valley, California, a variety of projects for San Francisco developer Fred R. Winn.

Geographic entities mentioned:
surface_form: Sonoma Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.3667
lon: -122.5
Goongerah, Victoria. Goongerah is a locality on the Brodribb River, located in Gippsland, Australia, near Mount Ellery. At the, Goongerah had a population of 31. Goongerah Post Office opened on 21 November 1952 and closed in 1974. Goongerah had one of the smallest primary schools in Victoria, with about 11 students. It closed in 2019.

Geographic entities mentioned:
surface_form: Mount Ellery
instance_of: Mountain
countries: Australia
coordinates: lat: -37.383333333333
lon: 148.8
Mount Agung. Mount Agung (,) is an active volcano in Karangasem Regency, Bali, Indonesia. It is located southeast of Mount Batur volcano, also in Bali. It is the highest point on Bali, and dominates the surrounding area, influencing the climate, especially rainfall patterns. From a distance, the mountain appears to be perfectly conical.

Geographic entities mentioned:
surface_form: Mount Batur
instance_of: Mountain
countries: Indonesia
coordinates: lat: -8.2419444444444
lon: 115.375
surface_form: batur
instance_of: Mountain
countries: Indonesia
coordinates: lat: -8.2419444444444
lon: 115.375
From a distance, the mountain appears to be perfectly conical. From the peak of the mountain, it is possible to see the peak of Mount Rinjani on the nearby island of Lombok, to the east, although both mountains are frequently covered in clouds. Agung is a stratovolcano, with a large and deep crater. Its most recent eruptions occurred from 2017–2019. 1963–64 eruption.

Geographic entities mentioned:
surface_form: Mount Rinjani
instance_of: Mountain
countries: Indonesia
coordinates: lat: -8.4166666666667
lon: 116.46666666667
surface_form: rinjani
instance_of: Mountain
countries: Indonesia
coordinates: lat: -8.4166666666667
lon: 116.46666666667
Of the 27 wildfires recorded in Bali's forests and savannas in September 2023, 13 – nearly half – occurred in the area surrounding Mount Agung in the Karangasem Regency; 5 fires were in the Buleleng Regency (northern part of the island) and 5 were near Mount Batur in the Bangli Regency. (Temperatures decrease from April to July, then rise again from August onward.)
Religious beliefs.

Geographic entities mentioned:
surface_form: Mount Batur
instance_of: Mountain
countries: Indonesia
coordinates: lat: -8.2419444444444
lon: 115.375
surface_form: batur
instance_of: Mountain
countries: Indonesia
coordinates: lat: -8.2419444444444
lon: 115.375
surface_form: agung
instance_of: Mountain
countries: Indonesia
coordinates: lat: -8.3419444444444
lon: 115.50777777778
surface_form: mount agung
instance_of: Mountain
countries: Indonesia
coordinates: lat: -8.3419444444444
lon: 115.50777777778
Mount Agung. Mount Agung (,) is an active volcano in Karangasem Regency, Bali, Indonesia. It is located southeast of Mount Batur volcano, also in Bali. It is the highest point on Bali, and dominates the surrounding area, influencing the climate, especially rainfall patterns. From a distance, the mountain appears to be perfectly conical.

Geographic entities mentioned:
surface_form: agung
instance_of: Mountain
countries: Indonesia
coordinates: lat: -8.3419444444444
lon: 115.50777777778
surface_form: mount agung
instance_of: Mountain
countries: Indonesia
coordinates: lat: -8.3419444444444
lon: 115.50777777778
From a distance, the mountain appears to be perfectly conical. From the peak of the mountain, it is possible to see the peak of Mount Rinjani on the nearby island of Lombok, to the east, although both mountains are frequently covered in clouds. Agung is a stratovolcano, with a large and deep crater. Its most recent eruptions occurred from 2017–2019. 1963–64 eruption.

Geographic entities mentioned:
surface_form: agung
instance_of: Mountain
countries: Indonesia
coordinates: lat: -8.3419444444444
lon: 115.50777777778
1963–64 eruption. The eruption of 1963 was one of the largest and most devastating eruptions in Indonesia's history. On February 18, 1963, local residents heard loud explosions and saw clouds rising from the crater of Mount Agung. On February 24, lava began flowing down the northern slope of the mountain, eventually traveling 7 km in the next 20 days.

Geographic entities mentioned:
surface_form: agung
instance_of: Mountain
countries: Indonesia
coordinates: lat: -8.3419444444444
lon: 115.50777777778
surface_form: mount agung
instance_of: Mountain
countries: Indonesia
coordinates: lat: -8.3419444444444
lon: 115.50777777778
By the beginning of December, the eruption reduced to minor emissions of steam and smoke. On 12 December, a picture of the crater was taken showing a steadily growing lava dome occupying approximately one third of the crater. In June 2018, Agung erupted with 2 km high plumes interrupting air traffic. On 3 July, a Strombolian explosion occurred, sending debris in all directions.

Geographic entities mentioned:
surface_form: agung
instance_of: Mountain
countries: Indonesia
coordinates: lat: -8.3419444444444
lon: 115.50777777778
Influence on the climate. In Bali, the wet or rainy season runs from November to March – but it does not wet the whole island equally. The mountain range of Gunung Agung creates a rain shadow that divides the island between a dry northern part (narrower) and a wet southern part (broader).

Geographic entities mentioned:
surface_form: agung
instance_of: Mountain
countries: Indonesia
coordinates: lat: -8.3419444444444
lon: 115.50777777778
surface_form: gunung agung
instance_of: Mountain
countries: Indonesia
coordinates: lat: -8.3419444444444
lon: 115.50777777778
(Temperatures decrease from April to July, then rise again from August onward.)
Religious beliefs. Balinese people believe that Mt Agung is a replica of Mt Meru, the central axis of the universe. The most important temple on Bali, Pura Besakih, is high on the slopes of Gunung Agung.

Geographic entities mentioned:
surface_form: agung
instance_of: Mountain
countries: Indonesia
coordinates: lat: -8.3419444444444
lon: 115.50777777778
(Temperatures decrease from April to July, then rise again from August onward.)
Religious beliefs. Balinese people believe that Mt Agung is a replica of Mt Meru, the central axis of the universe. The most important temple on Bali, Pura Besakih, is high on the slopes of Gunung Agung.

Geographic entities mentioned:
surface_form: agung
instance_of: Mountain
countries: Indonesia
coordinates: lat: -8.3419444444444
lon: 115.50777777778
surface_form: gunung agung
instance_of: Mountain
countries: Indonesia
coordinates: lat: -8.3419444444444
lon: 115.50777777778
Acraephia (Boeotia). Acraephia or Akraiphia (), Acraephiae or Akraiphiai (Ἀκραιφίαι), Acraephium or Akraiphion (Ἀκραίφιον), Acraephnium or Akraiphnion (Ἀκραίφνιον), was a town of ancient Boeotia on the slope of Mount Ptoum (Πτῶον) and on the eastern bank of the Lake Copais, which was here called Ἀκραιφὶς λίμνη from the town.

Geographic entities mentioned:
surface_form: Lake Copais
instance_of: Lake
countries: Greece
coordinates: lat: 38.45
lon: 23.05
The &quot;Kalomoira&quot; is said to have successfully partaken in several victorious battles under the command of the couple. Among other battles they took part in the campaign of Emmanouel Pappas in Chalkidiki and fought off the coasts of Athos, Lesbos and Samos.

Geographic entities mentioned:
surface_form: Athos
instance_of: Mountain
countries: Greece
coordinates: lat: 40.15833333333333
lon: 24.327222222222222
It is approximately 4,920 m high, reaching a prominence of at least 1,200 m. It is situated in the Oruro Department, Sabaya Province, Coipasa Municipality. The town of Coipasa lies on its northeastern side. An age of 3.7 million years has been inferred from the erosion status of the mountain, which shows evidence of Pleistocene glaciation.

Geographic entities mentioned:
surface_form: coipasa
instance_of: Lake
countries: Bolivia
coordinates: lat: -19.2
lon: -68.116666666667
Wila Pukarani. Wila Pukarani (Aymara &quot;wila&quot; red or blood, &quot;pukara&quot; pucará (fortress) or mountain of protection, &quot;-ni&quot; Aymara suffix to indicate ownership, &quot;the one with a red &quot;pukara&quot;, Hispanicized spellings &quot;Vila Pucarani&quot; / &quot;Villa Pucarani&quot;) is a volcano located in the Coipasa salt pan in the Bolivian Altiplano.

Geographic entities mentioned:
surface_form: wila pukarani
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.3306
lon: -68.3097
surface_form: pukarani
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.03
lon: -67.51861111
surface_form: pukarani
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.05055556
lon: -66.64527778
surface_form: pukarani
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.77666667
lon: -66.02138889
surface_form: pukarani
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.1414
lon: -68.4369
During the expedition through the tropical forest, his thoroughbred stallion died within a few days after a bite from a tsetse fly, many of his porters deserted, and the rest were decimated by tropical diseases. Stanley found David Livingstone on 10 November 1871 in Ujiji, near Lake Tanganyika in present-day Tanzania. He later claimed to have greeted him with the now-famous line, &quot;Dr.

Geographic entities mentioned:
surface_form: Lake Tanganyika
instance_of: Lake
countries: Tanzania
Democratic Republic of the Congo
Burundi
Zambia
coordinates: lat: -6.1
lon: 29.5
First trans-Africa expedition (1874–1877). In 1874, the &quot;New York Herald&quot; and the &quot;Daily Telegraph&quot; financed Stanley on another expedition to Africa. His ambitious objective was to complete the exploration and mapping of the Central African Great Lakes and rivers, in the process circumnavigating Lakes Victoria and Tanganyika and locating the source of the Nile.

Geographic entities mentioned:
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
surface_form: Victoria
instance_of: Lake
countries: Tanzania
Uganda
Kenya
coordinates: lat: -1
lon: 33
surface_form: Tanganyika
instance_of: Lake
countries: Tanzania
Democratic Republic of the Congo
Burundi
Zambia
coordinates: lat: -6.1
lon: 29.5
Founding of Leopoldville (Kinshasa). Stanley, who had left from a post at Vivi near Matadi on 21 February 1880, arrived at Stanley pool on 3 December 1882. Building a road from Vivi to Isangila, Stanley took almost 2 years to traverse the rapids towing with him 50 tonnes of equipment, including 2 dismantled steamboats and a barge.

Geographic entities mentioned:
surface_form: Stanley pool
instance_of: Lake
countries: Republic of the Congo
Democratic Republic of the Congo
coordinates: lat: -4.2819444444444
lon: 15.488611111111
King Leopold II demanded that Stanley take the longer route via the Congo River, hoping to acquire more territory and perhaps even Equatoria. After immense hardships and great loss of life, Stanley met Emin in 1888, mapped the Ruwenzori Range and Lake Edward, and emerged from the interior with Emin and his surviving followers at the end of 1890.

Geographic entities mentioned:
surface_form: Lake Edward
instance_of: Lake
countries: Uganda
Democratic Republic of the Congo
coordinates: lat: -0.33333333333333
lon: 29.6
Randle, Washington. Randle is a small town in eastern Lewis County, Washington, United States. Randle is located on U.S. Route 12 and is notable as the northeastern access point to the Mount St. Helens Windy Ridge viewpoint, by way of forest service roads that cut through the Gifford Pinchot National Forest.

Geographic entities mentioned:
surface_form: Mount St. Helens
instance_of: Mountain
countries: United States
coordinates: lat: 46.200277777778
lon: -122.18944444444
Leamy Lake. Leamy Lake (in French: &quot;Lac Leamy&quot;) is a lake in the Hull sector of Gatineau, Quebec, Canada. The lake is located just to the south of the Gatineau River, and just west of the Ottawa River, and is linked to both of them with flowing in from the Gatineau and exiting to the Ottawa. To the south is the Lac de la Carrière, a former quarry that is now a lake that is also linked.

Geographic entities mentioned:
surface_form: lac leamy
instance_of: Lake
countries: Canada
coordinates: lat: 45.451388888888886
lon: -75.72222222222223
surface_form: leamy lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.451388888888886
lon: -75.72222222222223
Leamy Lake. Leamy Lake (in French: &quot;Lac Leamy&quot;) is a lake in the Hull sector of Gatineau, Quebec, Canada. The lake is located just to the south of the Gatineau River, and just west of the Ottawa River, and is linked to both of them with flowing in from the Gatineau and exiting to the Ottawa. To the south is the Lac de la Carrière, a former quarry that is now a lake that is also linked.

Geographic entities mentioned:
surface_form: leamy lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.451388888888886
lon: -75.72222222222223
Geology. The Columbia Slough is part of the roughly Portland Basin, which lies at the northern end of the Willamette Valley of Oregon and extends north into Clark County in the state of Washington. The region is underlain by solidified lavas of the Columbia River Basalt Group that are up to 16 million years old.

Geographic entities mentioned:
surface_form: Willamette Valley
instance_of: Valley
countries: United States
coordinates: lat: 44.9
lon: -123.1
Water filled the entire Columbia Gorge to overflowing and turned the Willamette Valley into a lake long, wide and deep. The floodwaters ripped the face off Rocky Butte in Portland and deposited a gravel bar, Alameda Ridge, that runs parallel to and slightly south of the Columbia Slough. Faults associated with the expanding Portland Basin are capable of producing significant earthquakes.

Geographic entities mentioned:
surface_form: Rocky Butte
instance_of: Mountain
countries: United States
coordinates: lat: 45.546713888889
lon: -122.56594166667
Dhal Char is the southernmost island of Bhola district in Bangladesh. The island has attracted the attention of researchers, environmentalists and tourists alike for its unique position as one of the country's remotest permanently inhabited islands, far out in the Bay of Bengal. It also one of the most threatened pieces of land in the world as a result of rising sea levels, due to climate change.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
The nearest other bodies of land are Char Kukri Mukri to the northeast and Char Nizam to the west, both similar, albeit larger, islands. The eastern part of the island is witnessing rapid river bank erosion due to strong tidal flow of the Meghna as well as inclement weather in the Bay of Bengal.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
The eastern part of the island is witnessing rapid river bank erosion due to strong tidal flow of the Meghna as well as inclement weather in the Bay of Bengal. The island is marked as one of the most vulnerable areas for natural disasters and is regularly pummeled by cyclones in the northern Bay of Bengal ocean.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
St. Moritz-Celerina Olympic Bobrun. The Olympia Bob Run St. Moritz-Celerina is a bobsleigh track located in the Engadin Valley, Switzerland. It officially opened on New Year's Day 1904 and is the oldest bobsleigh track in the world. It is also the only one that is naturally refrigerated. It is used for other sliding sports, including skeleton and luge. History.

Geographic entities mentioned:
surface_form: Engadin Valley
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.5497
lon: 9.8959
Location. Lake Kanzigiri is on the boundary between the Commune of Bwambarangwe to the east and the Commune of Busoni to the west. It lies to the south of Lake Rweru, to which it is connected by an area of marshland. The settlement of Kabanga is to the west of its southern point, and the settlement of Bunwera is to the east of the same point. Mukenke is to the south.

Geographic entities mentioned:
surface_form: Lake Rweru
instance_of: Lake
countries: Rwanda
Burundi
coordinates: lat: -2.3777777777778
lon: 30.323611111111
Tributaries and outlet. The south end of the lake is a marsh that is fed by the Kanzigiri River and the Gacucu River, the lower part of the Kabuyenge River. The south end is also a marsh, and is fed by the Kanzigiri Lake and the Nyamabuno River, and empties into Lake Rweru. However, the direction of flow between Lake Rweru and Lake Kanzigiri depends on the time of year.

Geographic entities mentioned:
surface_form: Nyamabuno River
instance_of: Watercourse
countries: Burundi
coordinates: lat: -2.3958333333333
lon: 30.379166666667
surface_form: Lake Rweru
instance_of: Lake
countries: Rwanda
Burundi
coordinates: lat: -2.3777777777778
lon: 30.323611111111
surface_form: nyamabuno
instance_of: Watercourse
countries: Burundi
coordinates: lat: -2.3958333333333
lon: 30.379166666667
Lake Kanzigiri. Lake Kanzigiri (,) is a lake in the Kirundo Province of Burundi. Location. Lake Kanzigiri is on the boundary between the Commune of Bwambarangwe to the east and the Commune of Busoni to the west. It lies to the south of Lake Rweru, to which it is connected by an area of marshland.

Geographic entities mentioned:
surface_form: lake kanzigiri
instance_of: Lake
countries: Burundi
coordinates: lat: -2.4583333333333
lon: 30.3625
The settlement of Kabanga is to the west of its southern point, and the settlement of Bunwera is to the east of the same point. Mukenke is to the south. Around Lake Kanzigiri there are wooded savannahs dominated by plants such as &quot;Pericopsis angolensis&quot;, &quot;Parinari curatellifolia&quot; and &quot;Hymenocardia acida&quot;, which indicate Zambezian influences.

Geographic entities mentioned:
surface_form: lake kanzigiri
instance_of: Lake
countries: Burundi
coordinates: lat: -2.4583333333333
lon: 30.3625
These eastern savannas are mainly found in the Ruvubu National Park, which indicates that Lake Kanzigiri and its marshes associated with it are a zone of separation between the Bugesera District and the Mosso-Malagarazi District. Tributaries and outlet. The south end of the lake is a marsh that is fed by the Kanzigiri River and the Gacucu River, the lower part of the Kabuyenge River.

Geographic entities mentioned:
surface_form: lake kanzigiri
instance_of: Lake
countries: Burundi
coordinates: lat: -2.4583333333333
lon: 30.3625
The south end is also a marsh, and is fed by the Kanzigiri Lake and the Nyamabuno River, and empties into Lake Rweru. However, the direction of flow between Lake Rweru and Lake Kanzigiri depends on the time of year. At the start of the rainy season, Lake Rweru flows towards the Kagera River.

Geographic entities mentioned:
surface_form: lake kanzigiri
instance_of: Lake
countries: Burundi
coordinates: lat: -2.4583333333333
lon: 30.3625
However, the direction of flow between Lake Rweru and Lake Kanzigiri depends on the time of year. At the start of the rainy season, Lake Rweru flows towards the Kagera River. By March–April, the Kagera river level is higher than that of Lake Rweru, and the flow is reversed, with the river flowing into Lake Rweru and the marshes that surround it, including that leading to Lake Kanzigiri.

Geographic entities mentioned:
surface_form: lake kanzigiri
instance_of: Lake
countries: Burundi
coordinates: lat: -2.4583333333333
lon: 30.3625
When the flood recedes, between June and August, Lake Rweru flows towards the Nyabarongo River over the swamp, and later through a single channel. Ecosystem. The Kabuyenge Marsh and the Kabanga Marsh maintain the hydrological balance of Lake Kanzigiri. The United Nations Food and Agriculture Organization (FAO) had developed buffer zones around each of these marshes.

Geographic entities mentioned:
surface_form: lake kanzigiri
instance_of: Lake
countries: Burundi
coordinates: lat: -2.4583333333333
lon: 30.3625
The United Nations Food and Agriculture Organization (FAO) had developed buffer zones around each of these marshes. If the papyrus swamp between Lake Kanzigiri and Lake Rweru were drained, Lake Kanzigiri would dry up during the low flow period. The swamp ecosystem is threatened by uncontrolled extension of farming into the swamps, and also by the recent droughts.

Geographic entities mentioned:
surface_form: lake kanzigiri
instance_of: Lake
countries: Burundi
coordinates: lat: -2.4583333333333
lon: 30.3625
Tributaries and outlet. The south end of the lake is a marsh that is fed by the Kanzigiri River and the Gacucu River, the lower part of the Kabuyenge River. The south end is also a marsh, and is fed by the Kanzigiri Lake and the Nyamabuno River, and empties into Lake Rweru. However, the direction of flow between Lake Rweru and Lake Kanzigiri depends on the time of year.

Geographic entities mentioned:
surface_form: kabuyenge river
instance_of: Watercourse
countries: Burundi
coordinates: lat: -2.5869444444444
lon: 30.305833333333
Granite Dells. The Granite Dells is a geological feature north of Prescott, Arizona. The Dells consist of exposed bedrock and large boulders of granite that have eroded into an unusual lumpy, rippled appearance. Watson Lake and Willow Lake are small man-made reservoirs in this formation.

Geographic entities mentioned:
surface_form: granite dells
instance_of: Landform
countries: United States
coordinates: lat: 34.6147
lon: -112.418
Watson Lake and Willow Lake are small man-made reservoirs in this formation. The Peavine National Recreation Trail follows the former railbed of the Santa Fe, Prescott and Phoenix Railway through the Granite Dells. This winding portion of the railroad was known as the &quot;Peavine&quot; because its twisting curves resembled that of a pea vine.

Geographic entities mentioned:
surface_form: granite dells
instance_of: Landform
countries: United States
coordinates: lat: 34.6147
lon: -112.418
This winding portion of the railroad was known as the &quot;Peavine&quot; because its twisting curves resembled that of a pea vine. It connects to the Iron King Trail, which follows the route of the old Prescott & Eastern Railroad through the eastern Granite Dells. Both are rail trail conversions. Geology. The Precambrian Dells granite has been radiometrically dated at 1.4 billion years old.

Geographic entities mentioned:
surface_form: granite dells
instance_of: Landform
countries: United States
coordinates: lat: 34.6147
lon: -112.418
Its pluton was intruded at a depth of around one or two miles (1.6 to 3.2 km). These cover rocks have since been eroded away. Weathering along joints produced the rounded boulders and other unusual rock formations that characterize the Granite Dells. This process is called spheroidal weathering, and is common in granitic terrains.

Geographic entities mentioned:
surface_form: granite dells
instance_of: Landform
countries: United States
coordinates: lat: 34.6147
lon: -112.418
He also hosted shows in New York City at 710 WOR and at TheBlaze Radio Network. Early life. Severin was born in the Hudson Valley region of New York State. His mother was a writer and his father was a direct mail advertising entrepreneur. He spent at least a portion of his childhood and teen years in Poughkeepsie, New York where he founded his sixth grade civics club and school newspaper.

Geographic entities mentioned:
surface_form: Hudson Valley
instance_of: Valley
countries: United States
coordinates: lat: 41.9209
lon: -73.9613
Similarly, the Annapurna Conservation Area Project (ACAP), the Manaslu Conservation Area Project (MCAP) and Gaurishankar Conservation Area Project (GCAP) are three protected areas managed by the Trust in the mountain region. The Central Zoo is the only project of the Trust in Kathmandu valley.

Geographic entities mentioned:
surface_form: Kathmandu valley
instance_of: Valley
countries: Nepal
coordinates: lat: 27.703944444444
lon: 85.308583333333
By the 1970s, the station had dropped fine arts programming in favor of what became known as adult contemporary music, which is roughly its present format. (Public radio station WLRH took over classical broadcasting to the area when it began in 1976.)
After nearly 40 years serving the Tennessee Valley, Hornbuckle retired, selling the station in July 1999.

Geographic entities mentioned:
surface_form: Tennessee Valley
instance_of: Valley
countries: United States
coordinates: lat: 35.959166666667
lon: -83.850277777778
At Jamestown, it passes the world's largest sculpture of a buffalo (actually bison) named &quot;Dakota Thunder&quot;, in height and on the north of the highway. At approximately milemarker 275 on the westbound lanes between Jamestown and Valley City, the highway crosses the Laurentian Divide, at an elevation of above sea level.

Geographic entities mentioned:
surface_form: Laurentian Divide
instance_of: Landform
countries: United States
Canada
When Kintetsu acquired the line the following year, it was relatively painless to tie the two lines together and it soon began offering limited express service directly from in Osaka and to Yunoyama, aimed at attracting tourists to the onsen and nearby Mount Gozaisho. This service was offered for over 30 years but was ceased in 1998 due to insufficient ridership.

Geographic entities mentioned:
surface_form: Mount Gozaisho
instance_of: Mountain
countries: Japan
coordinates: lat: 35.02027
lon: 136.41945
Lilla sjö (Hästveda socken, Skåne). Lilla Sjö is a lake in the municipality of Hässleholm in Skåne and is part of the main catchment area of the Helge River. The lake has an area of 0.144 square kilometers and has an elevation of 57.6 meters above sea level.

Geographic entities mentioned:
surface_form: lilla sjö (hästveda socken, skåne)
instance_of: Lake
countries: Sweden
coordinates: lat: 56.2816
lon: 13.9242
Lilla sjö (Hästveda socken, Skåne). Lilla Sjö is a lake in the municipality of Hässleholm in Skåne and is part of the main catchment area of the Helge River. The lake has an area of 0.144 square kilometers and has an elevation of 57.6 meters above sea level.

Geographic entities mentioned:
surface_form: lilla sjö
instance_of: Lake
countries: Sweden
coordinates: lat: 56.2816
lon: 13.9242
However, due to the lack of a functional wastewater treatment plant, non-existent filtration from peat mining at Åbuamossen, and phosphorus and nitrogen leaks from households and agriculture, it became difficult for the lake to survive on its own. There is a 2.6 km long illuminated exercise trail around Lilla Sjö.

Geographic entities mentioned:
surface_form: lilla sjö
instance_of: Lake
countries: Sweden
coordinates: lat: 56.2816
lon: 13.9242
Beaver Lake (Yarmouth). Beaver Lake Yarmouth is a lake of Yarmouth District, in Nova Scotia, Canada.

Geographic entities mentioned:
surface_form: beaver lake
instance_of: Lake
countries: Canada
coordinates: lat: 46.7183
lon: -60.5103
surface_form: beaver lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.4987
lon: -73.59742
surface_form: beaver lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.7058
lon: -111.816
surface_form: beaver lake (yarmouth)
instance_of: Lake
countries: Canada
coordinates: lat: 44.0001
lon: -66.1432
surface_form: beaver lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.8333
lon: -102.301
surface_form: beaver lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.351
lon: -62.496
surface_form: beaver lake
instance_of: Lake
countries: Canada
coordinates: lat: 43.8191
lon: -65.5396
surface_form: beaver lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.2596
lon: -65.2402
Beaver Lake (Yarmouth). Beaver Lake Yarmouth is a lake of Yarmouth District, in Nova Scotia, Canada.

Geographic entities mentioned:
surface_form: beaver lake
instance_of: Lake
countries: Canada
coordinates: lat: 46.7183
lon: -60.5103
surface_form: beaver lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.4987
lon: -73.59742
surface_form: beaver lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.7058
lon: -111.816
surface_form: beaver lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.0001
lon: -66.1432
surface_form: beaver lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.8333
lon: -102.301
surface_form: beaver lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.351
lon: -62.496
surface_form: beaver lake
instance_of: Lake
countries: Canada
coordinates: lat: 43.8191
lon: -65.5396
surface_form: beaver lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.2596
lon: -65.2402
Kashmir, Hazara, Nuristan, Laghman, Azad Kashmir, Jammu, Himachal Pradesh, Ladakh, Gilgit Baltistan, Chitral, Western Tibet, Western Xinjiang, Badakhshan, Gorno Badakhshan, Fergana, Osh and Turkistan Region.

Geographic entities mentioned:
surface_form: Chitral
instance_of: Valley
countries: Pakistan
coordinates: lat: 35.85111111111111
lon: 71.78888888888889
Kafr Manda. Northern
Kafr Manda or Kfar Menda (,) is an Arab town in the Lower Galilee, on the slopes of Mount Atzmon in Israel's Northern District. Kafr Manda is northwest of the city of Nazareth. In its population was. The inhabitants are predominantly Arab Muslims. Classical antiquity. Kafr Manda is located on an ancient site on a low hill.

Geographic entities mentioned:
surface_form: Mount Atzmon
instance_of: Mountain
countries: Israel
coordinates: lat: 32.8238889
lon: 35.2666667
In 1954, the Nelson-Atkins Museum of Art held an exhibition of his work in their main loan gallery. After the mid-1950s, James lost interest in promoting his work on a national stage, but he continued his prolific output, producing many watercolors of rural Missouri and Kansas, especially the Flint Hills of Kansas.

Geographic entities mentioned:
surface_form: Flint Hills
instance_of: Landform
countries: United States
coordinates: lat: 37.2833
lon: -96.6753
It is located in the La Paz Department, Inquisivi Province, Colquiri Municipality. It lies southwest of Kuntur Samaña and southeast of Iru Pata. The peak northeast of Jach'a Warmi Qullu is named Warmi Qullu. It has the same height.

Geographic entities mentioned:
surface_form: Iru Pata
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.52972222
lon: -66.94888889
surface_form: iru pata
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.52972222
lon: -66.94888889
Jach'a Warmi Qullu. Jach'a Warmi Qullu (Aymara &quot;jach'a&quot; big, &quot;warmi&quot; woman, &quot;qullu&quot; mountain, &quot;big woman's mountain&quot;, also spelled &quot;Jachcha Huarmi Kkollu&quot;) is a mountain in the Bolivian Andes. It is located in the La Paz Department, Inquisivi Province, Colquiri Municipality. It lies southwest of Kuntur Samaña and southeast of Iru Pata.

Geographic entities mentioned:
surface_form: jach'a warmi qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.54333333
lon: -66.93638889
Bern–Lucerne railway. The Bern–Lucerne railway is a partially double-track, electrified railway through the Entlebuch in Switzerland. The main section between Langnau and Gütsch near Lucerne was opened on 11 August 1875. History.

Geographic entities mentioned:
surface_form: Entlebuch
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.75
lon: 7.8
Worth Valley (dale). The Worth Valley is a geographic area in West Yorkshire, England, that extends eastwards from Crow Hill and Oxenhope Moor, providing drainage for the River Worth for nearly to the River Aire. It is a side valley to Airedale, with the River Worth being a major tributary of the River Aire.

Geographic entities mentioned:
surface_form: Airedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.017
lon: -1.465
Connected with these attractions has been the film and TV industry which have recorded shots, programmes, and entire films in the area. History. In the period when Airedale was subject to glaciation, lakes developed in the valleys which held water behind ice sheets. The emptying and melting of the Airedale Glacier is believed to have carved out Airedale, Bradford Dale and the Worth Valley.

Geographic entities mentioned:
surface_form: bradford dale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.794
lon: -1.7632
surface_form: worth valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.831
lon: -1.956
surface_form: airedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.017
lon: -1.465
surface_form: airedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.017
lon: -1.465
The naming of the valley does not follow the convention of other river valleys in West Yorkshire, (Airedale, Bradford Dale, Calderdale etc). However, some buildings in Keighley, at the end of the Worth Valley, were given the name Worthdale.

Geographic entities mentioned:
surface_form: bradford dale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.794
lon: -1.7632
surface_form: airedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.017
lon: -1.465
Worth Valley (dale). The Worth Valley is a geographic area in West Yorkshire, England, that extends eastwards from Crow Hill and Oxenhope Moor, providing drainage for the River Worth for nearly to the River Aire. It is a side valley to Airedale, with the River Worth being a major tributary of the River Aire.

Geographic entities mentioned:
surface_form: worth valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.831
lon: -1.956
It is a side valley to Airedale, with the River Worth being a major tributary of the River Aire. The Worth Valley was important for its contribution to the textiles industry of the West Riding of Yorkshire and was furnished with several reservoirs to allow mills to operate within the valley. Most of the reservoirs are still in use into the modern day.

Geographic entities mentioned:
surface_form: worth valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.831
lon: -1.956
Most of the reservoirs are still in use into the modern day. The valley has seen a shift in its industry from worsted, wool, and before that mining and quarrying, into a tourist location. The association with the Brontë family, and the Keighley and Worth Valley Railway, has drawn many visitors to the area, particularly from Japan.

Geographic entities mentioned:
surface_form: worth valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.831
lon: -1.956
The emptying and melting of the Airedale Glacier is believed to have carved out Airedale, Bradford Dale and the Worth Valley. The Worth Valley actually had two lakes, one in the Worth Valley itself near to Stanbury (known as &quot;Lake Worth&quot;, and a second long, narrow lake south of Oxenhope (known as &quot;Oxenhope Lake&quot;).

Geographic entities mentioned:
surface_form: worth valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.831
lon: -1.956
surface_form: worth valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.831
lon: -1.956
Later still, with water draining eastward from what is now Lancashire, and the wash of the water cutting away at the ridges, the two lakes merged into one which had three arms stretching up the Sladen Valley, the Upper Worth Valley and the valley towards Oxenhope that is now drained by Bridgehouse Beck.

Geographic entities mentioned:
surface_form: worth valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.831
lon: -1.956
The naming of the valley does not follow the convention of other river valleys in West Yorkshire, (Airedale, Bradford Dale, Calderdale etc). However, some buildings in Keighley, at the end of the Worth Valley, were given the name Worthdale.

Geographic entities mentioned:
surface_form: worth valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.831
lon: -1.956
surface_form: worth valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.831
lon: -1.956
However, some buildings in Keighley, at the end of the Worth Valley, were given the name Worthdale. Whilst the Worth Valley extends from Watersheddles Reservoir to the Stockbridge part of Keighley, the area known as the Worth Valley also encompasses North Beck and Bridgehouse Beck, which are due north and due south of the River Worth respectively.

Geographic entities mentioned:
surface_form: worth valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.831
lon: -1.956
In terms of Geomorphology, the Worth Valley is described as being between Oxenhope and Keighley, as well as the Upper Worth valley up to Ponden and Watersheddles Reservoirs. Since the Middle Ages, sheep farming dominated, especially in the lower parts of the valley floors, and hand-looming became a notable way of earning a second wage.

Geographic entities mentioned:
surface_form: worth valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.831
lon: -1.956
surface_form: worth valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.831
lon: -1.956
The River Worth runs for from Watersheddles to the River Aire at Aireworth, a suburb of Keighley. Haworth and Oxenhope are considered to be in the Worth Valley, although strictly speaking, there are in the vale cut by Bridgehouse Beck (sometimes referred to as Oxenhope Beck). The beck enters the River Worth at Mytholmes. Geology.

Geographic entities mentioned:
surface_form: worth valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.831
lon: -1.956
The beck enters the River Worth at Mytholmes. Geology. The underlying geology of the area is the Namurian millstone grit series which extends into Airedale. Coal reserves were found in thin beds in the Worth valley, but the arrival of the railways in the area meant that cheaper and better quality coal could be railed in from the Yorkshire coalfields.

Geographic entities mentioned:
surface_form: worth valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.831
lon: -1.956
This stone had a blueish-grey colour when first exposed and was very resistant to wear and so was used to dress roads in the turnpike era. Most of the sandstone quarried in the area was used for building, especially the woollen and worsted mills in the Worth Valley and beyond.

Geographic entities mentioned:
surface_form: worth valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.831
lon: -1.956
These areas are the major water catchments, and the peat can lead to discolouration of the water. The water catchment areas on the moors are part of the South Pennine Moors SSSI. At Crow Hill, on the western extremity of the Worth Valley, a bog burst in 1824, which saw the Brontë children having to take shelter in Ponden Hall. Industry.

Geographic entities mentioned:
surface_form: worth valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.831
lon: -1.956
Industry. The combination of the availability of water, and the proximity to the Lancashire worsted, wool and cotton industries, helped the Worth valley thrive as an industrial region in the late 18th/early 19th centuries. Many of the reservoirs in the upper valleys were built as compensation reservoirs to keep a constant flow of water available in the River Worth, feeding the mills downstream.

Geographic entities mentioned:
surface_form: worth valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.831
lon: -1.956
This was proposed in 1846 and never taken up, but the line which eventually became the Keighley and Worth Valley Railway, was built in the 1860s after local businessmen petitioned the Midland Railway headquarters in Derby. As the line is now a heritage railway, the nearest public railway station is at, and the nearest airport to Haworth (Leeds Bradford Airport) is away to the east.

Geographic entities mentioned:
surface_form: worth valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.831
lon: -1.956
As the line is now a heritage railway, the nearest public railway station is at, and the nearest airport to Haworth (Leeds Bradford Airport) is away to the east. A second railway was built by the Great Northern Railway which left Keighley along the same line as the Worth Valley but followed the contours of the valley on the south side to breach the hill via a curved tunnel (Lees Moor) and go into.

Geographic entities mentioned:
surface_form: worth valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.831
lon: -1.956
surface_form: worth valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.831
lon: -1.956
A second railway was built by the Great Northern Railway which left Keighley along the same line as the Worth Valley but followed the contours of the valley on the south side to breach the hill via a curved tunnel (Lees Moor) and go into. Several footpaths cross the Worth Valley;
Culture. The Worth Valley is synonymous with the Brontë family.

Geographic entities mentioned:
surface_form: worth valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.831
lon: -1.956
Connected with these attractions has been the film and TV industry which have recorded shots, programmes, and entire films in the area. History. In the period when Airedale was subject to glaciation, lakes developed in the valleys which held water behind ice sheets. The emptying and melting of the Airedale Glacier is believed to have carved out Airedale, Bradford Dale and the Worth Valley.

Geographic entities mentioned:
surface_form: airedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.017
lon: -1.465
The beck enters the River Worth at Mytholmes. Geology. The underlying geology of the area is the Namurian millstone grit series which extends into Airedale. Coal reserves were found in thin beds in the Worth valley, but the arrival of the railways in the area meant that cheaper and better quality coal could be railed in from the Yorkshire coalfields.

Geographic entities mentioned:
surface_form: airedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.017
lon: -1.465
Société électrique Vevey-Montreux SA (SEVM). In 1878, Adolphe Dupraz and Henri Chaudet first applied to the canton for a concession to operate the, a stream that flows from the Rochers de Naye to the town of Montreux. The two entrepreneurs wanted to create an electric tramway line between Vevey and Montreux.

Geographic entities mentioned:
surface_form: Rochers de Naye
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.431944444444
lon: 6.9761666666667