Sarmila/GeoWiki-Features huggingface dataset:
The edifice has a volume of about and covers a surface area of about. Radial valleys extend away from the top. A number of particular landforms on Sollipulli formed under the influence of glacial ice, such as the caldera structure. The Nevados de Sollipulli mountain chain west of the Sollipulli caldera are a chain of volcanoes which is heavily eroded.

Geographic entities mentioned:
surface_form: sollipulli
instance_of: Mountain
countries: Chile
coordinates: lat: -38.975
lon: -71.52
Radial valleys extend away from the top. A number of particular landforms on Sollipulli formed under the influence of glacial ice, such as the caldera structure. The Nevados de Sollipulli mountain chain west of the Sollipulli caldera are a chain of volcanoes which is heavily eroded. They are formed by breccia and lava flows; glacial action has left cirques.

Geographic entities mentioned:
surface_form: sollipulli
instance_of: Mountain
countries: Chile
coordinates: lat: -38.975
lon: -71.52
surface_form: sollipulli
instance_of: Mountain
countries: Chile
coordinates: lat: -38.975
lon: -71.52
These glaciers drain to the north and northwest; the latter glacier flows from the caldera through the Alpehué crater into the valley of the same name, which is drained by the Rio Alpehué into the Rio Allipén river. Other than the caldera and crater glaciers, the only snow cover on Sollipulli is seasonal.

Geographic entities mentioned:
surface_form: sollipulli
instance_of: Mountain
countries: Chile
coordinates: lat: -38.975
lon: -71.52
Glaciers have been present on the volcano before the Last Glacial Maximum and have left glacial valleys on its slopes, glacial striations and evidence of subglacial eruptions such as hyaloclastite deposits. The glacier within the caldera of Sollipulli is shrinking; its surface area decreased between 1961 and 2011 and the Alpehuén outlet glacier retreated by.

Geographic entities mentioned:
surface_form: sollipulli
instance_of: Mountain
countries: Chile
coordinates: lat: -38.975
lon: -71.52
The glacier within the caldera of Sollipulli is shrinking; its surface area decreased between 1961 and 2011 and the Alpehuén outlet glacier retreated by. There is evidence that the equilibrium line altitude has risen above the volcano. Some smaller ice fields around Sollipulli either shrank between 1986 and 2017 or disappeared altogether.

Geographic entities mentioned:
surface_form: sollipulli
instance_of: Mountain
countries: Chile
coordinates: lat: -38.975
lon: -71.52
Sollipulli volcano developed on a basement which consists of the Jurassic–Cretaceous Nacientes del Biobío formation and the Pliocene-Pleistocene Nevados de Sollipulli volcanics, with subordinate exposures of the Miocene Curamallín and the Cretaceous-Tertiary Vizcacha-Cumilao complex volcano-sedimentary formations. Miocene granites are intruded into the basement.

Geographic entities mentioned:
surface_form: sollipulli
instance_of: Mountain
countries: Chile
coordinates: lat: -38.975
lon: -71.52
surface_form: sollipulli
instance_of: Mountain
countries: Chile
coordinates: lat: -38.975
lon: -71.52
Miocene granites are intruded into the basement. Two major fault systems, the Liquiñe-Ofqui Fault Zone and the Reigolil-Pirihueico fault, pass west and east of Sollipulli, respectively. They are connected by eastwest trending faults
Composition. Rocks erupted from Sollipulli range from basalt over basaltic andesite and andesite to dacite.

Geographic entities mentioned:
surface_form: sollipulli
instance_of: Mountain
countries: Chile
coordinates: lat: -38.975
lon: -71.52
They are connected by eastwest trending faults
Composition. Rocks erupted from Sollipulli range from basalt over basaltic andesite and andesite to dacite. Composition has changed over the evolution of the volcano; sometimes one type of rock is found as inclusion in another.

Geographic entities mentioned:
surface_form: sollipulli
instance_of: Mountain
countries: Chile
coordinates: lat: -38.975
lon: -71.52
Obsidian was obtained on Sollipulli and exported over large distances; it has been found as far as Argentina's steppes and northern Chile, and is chemically and in appearance different from obsidian obtained on Chaitén volcano. One source has been identified at a lava dome on the western side of Sollipulli.

Geographic entities mentioned:
surface_form: sollipulli
instance_of: Mountain
countries: Chile
coordinates: lat: -38.975
lon: -71.52
Eruption history. Sollipulli was active during the Pleistocene and Holocene; the Nevados de Sollipulli are less than 1.8 million years old with argon-argon dating having obtained ages of 490,000 ± 30,000 and 312,000 ±  20,000 years ago. Six separate volcanic units form the edifice; from the oldest to the youngest they are the Sharkfin, Northwest, South, Peak, Alpehué and Chufquén units.

Geographic entities mentioned:
surface_form: sollipulli
instance_of: Mountain
countries: Chile
coordinates: lat: -38.975
lon: -71.52
Alpehué tephra has been used as a tephrochronology tool. Pyroclastic flows from the eruption melted the caldera ice sheet, forming lahars that propagated northwest away from Sollipulli. Ignimbrites from this eruption cover surfaces of at least around Sollipulli, their volume has been estimated to be about.

Geographic entities mentioned:
surface_form: sollipulli
instance_of: Mountain
countries: Chile
coordinates: lat: -38.975
lon: -71.52
Pyroclastic flows from the eruption melted the caldera ice sheet, forming lahars that propagated northwest away from Sollipulli. Ignimbrites from this eruption cover surfaces of at least around Sollipulli, their volume has been estimated to be about. They are brown to grey in colour and unwelded with the exception of part of the ignimbrite that is emplaced within the Alpehué crater.

Geographic entities mentioned:
surface_form: sollipulli
instance_of: Mountain
countries: Chile
coordinates: lat: -38.975
lon: -71.52
This eruption deposited ash onto the caldera ice, while it is absent from the central parts of the Chufquén valley; either it was removed by a later glacier advance or it landed on a glacier which later retreated. The eruption occurred relatively recently, indicating that Sollipulli is still active. Presently, fumaroles and geothermal phenomena occur at the northwestern foot of Sollipulli.

Geographic entities mentioned:
surface_form: sollipulli
instance_of: Mountain
countries: Chile
coordinates: lat: -38.975
lon: -71.52
The eruption occurred relatively recently, indicating that Sollipulli is still active. Presently, fumaroles and geothermal phenomena occur at the northwestern foot of Sollipulli. The Alpehue geothermal field, about southwest of Alpehue crater, is unusual among the southern Chilean geothermal fields as it features geysers.

Geographic entities mentioned:
surface_form: sollipulli
instance_of: Mountain
countries: Chile
coordinates: lat: -38.975
lon: -71.52
The Alpehue geothermal field, about southwest of Alpehue crater, is unusual among the southern Chilean geothermal fields as it features geysers. It lies within a glacial valley presently traversed by the Allipén River, which has cut a vertical canyon into the Nevados de Sollipulli volcano, close to the intersection between two faults.

Geographic entities mentioned:
surface_form: sollipulli
instance_of: Mountain
countries: Chile
coordinates: lat: -38.975
lon: -71.52
Hazards. The substantial ice body in the caldera means that there is a significant risk of mudflows or glacier bursts in the case of renewed activity. Conversely, a retreat of the caldera-filling glacier might facilitate the onset of explosive eruptions at Sollipulli. A repeat of the Alpehué eruption would be a regional catastrophe, comparable to the 1991 eruption of Cerro Hudson volcano.

Geographic entities mentioned:
surface_form: sollipulli
instance_of: Mountain
countries: Chile
coordinates: lat: -38.975
lon: -71.52
About 60 volcanoes have erupted in historical time in the Andes, and 118 additional volcanic systems show evidence of Holocene eruptions. There are 60 volcanoes in the Southern Volcanic Zone; among these are Cerro Azul and Cerro Hudson, which experienced large eruptions in 1932 and 1991 that resulted in the emission of substantial volumes of ash.

Geographic entities mentioned:
surface_form: cerro azul
instance_of: Mountain
countries: Chile
coordinates: lat: -35.653333333333
lon: -70.760833333333
surface_form: cerro hudson
instance_of: Mountain
countries: Chile
coordinates: lat: -45.92
lon: -72.95
The Sollipulli volcano is in the western part of the Nevados de Sollipulli mountain range, which is bordered to the north, south and east by river valleys. The communes of Curarrehue, Cunco, Panguipulli, Pucón and Villarrica are in the area, Melipeuco lies northwest. The volcano is also part of the Kütralkura geopark project. Regional.

Geographic entities mentioned:
surface_form: villarrica
instance_of: Mountain
countries: Chile
coordinates: lat: -39.42
lon: -71.939166666667
surface_form: villarrica
instance_of: Lake
countries: Chile
coordinates: lat: -39.25
lon: -72.083333333333
Conversely, a retreat of the caldera-filling glacier might facilitate the onset of explosive eruptions at Sollipulli. A repeat of the Alpehué eruption would be a regional catastrophe, comparable to the 1991 eruption of Cerro Hudson volcano. The Chilean geological service Sernageomin monitors the volcano and publishes a hazard index for it.

Geographic entities mentioned:
surface_form: hudson volcano
instance_of: Mountain
countries: Chile
coordinates: lat: -45.92
lon: -72.95
surface_form: cerro hudson
instance_of: Mountain
countries: Chile
coordinates: lat: -45.92
lon: -72.95
2008 UCI Mountain Bike & Trials World Championships. The 2008 UCI Mountain Bike & Trials World Championships were held in Val di Sole, Italy from 17 to 22 June 2008. The disciplines included were cross-country, downhill, four-cross, and trials. The event was the 19th edition of the UCI Mountain Bike World Championships and the 23rd edition of the UCI Trials World Championships.

Geographic entities mentioned:
surface_form: Val di Sole
instance_of: Valley
countries: Italy
coordinates: lat: 46.3
lon: 10.8
Dolon Pass. Dolon Pass () is a pass located between the Songköl Too and the Bayduluu Range in Naryn Region, Kyrgyzstan. The pass lies at. Highway of international significance ЭМ-11 (as per the national road classification) connecting Bishkek, Balykchy, Naryn, Torugart, and Kyrgyzstan-China border, which is also known as European route E125 and Asian Highway 61 in Kyrgyzstan, traverses the pass.

Geographic entities mentioned:
surface_form: Songköl Too
instance_of: Mountain
countries: Kyrgyzstan
coordinates: lat: 41.877886
lon: 75.545176
Lake Iroquois (formerly known as Hinesburg pond) was created in 1867 to supply mills in Hinesburg with a better water supply. Building a dam on Pond Brook caused the existing spring-fed pond to rise above its banks and become the current lake. The towns share a beach on the lake, plus there is a public boat access.

Geographic entities mentioned:
surface_form: current lake
instance_of: Lake
countries: United States
coordinates: lat: 44.164444444444
lon: -95.946388888889
There are also several streams that bubble up from the lake bottom. The outflow of the lake is over the dam in the south end. The outlet stream flows into Sunset Lake in Hinesburg, and then into the LaPlatte River and into Lake Champlain. The lake is used extensively throughout the year by residents and by visitors.

Geographic entities mentioned:
surface_form: sunset lake
instance_of: Lake
countries: United States
coordinates: lat: 42.2029626
lon: -71.0124654
surface_form: sunset lake
instance_of: Lake
countries: United States
coordinates: lat: 43.4722
lon: -71.3044
surface_form: sunset lake
instance_of: Lake
countries: United States
coordinates: lat: 28.53635
lon: -81.41141
surface_form: sunset lake
instance_of: Lake
countries: United States
coordinates: lat: 35.648888888889
lon: -78.791388888889
surface_form: sunset lake
instance_of: Lake
countries: United States
coordinates: lat: 44.544722222222
lon: -89.277222222222
Lake Iroquois (Vermont). Lake Iroquois is a reservoir in northwestern Vermont, bordered by three towns: Hinesburg, Williston, and Richmond. Lake Iroquois (formerly known as Hinesburg pond) was created in 1867 to supply mills in Hinesburg with a better water supply. Building a dam on Pond Brook caused the existing spring-fed pond to rise above its banks and become the current lake.

Geographic entities mentioned:
surface_form: lake iroquois
instance_of: Lake
countries: United States
coordinates: lat: 40.5291
lon: -88.0932
surface_form: lake iroquois (vermont)
instance_of: Lake
countries: United States
coordinates: lat: 44.3708
lon: -73.0844
surface_form: lake iroquois
instance_of: Lake
countries: United States
coordinates: lat: 44.34916667
lon: -97.83222222
Lake Iroquois (Vermont). Lake Iroquois is a reservoir in northwestern Vermont, bordered by three towns: Hinesburg, Williston, and Richmond. Lake Iroquois (formerly known as Hinesburg pond) was created in 1867 to supply mills in Hinesburg with a better water supply. Building a dam on Pond Brook caused the existing spring-fed pond to rise above its banks and become the current lake.

Geographic entities mentioned:
surface_form: lake iroquois
instance_of: Lake
countries: United States
coordinates: lat: 40.5291
lon: -88.0932
surface_form: lake iroquois
instance_of: Lake
countries: United States
coordinates: lat: 44.3708
lon: -73.0844
surface_form: lake iroquois
instance_of: Lake
countries: United States
coordinates: lat: 44.34916667
lon: -97.83222222
The outlet stream flows into Sunset Lake in Hinesburg, and then into the LaPlatte River and into Lake Champlain. The lake is used extensively throughout the year by residents and by visitors. The Lake Iroquois Recreation District (LIRD) maintains the public beach at the north end of the lake. The LIRD also maintains a trail network on the land around the lake.

Geographic entities mentioned:
surface_form: lake iroquois
instance_of: Lake
countries: United States
coordinates: lat: 40.5291
lon: -88.0932
surface_form: lake iroquois
instance_of: Lake
countries: United States
coordinates: lat: 44.3708
lon: -73.0844
surface_form: lake iroquois
instance_of: Lake
countries: United States
coordinates: lat: 44.34916667
lon: -97.83222222
The Vermont Department of Fish and Wildlife maintains the fishing access and boat ramp, also at the north end of the lake, which provides public access to the lake for boating and fishing. Drainage Basin Area: 2, 418 acres
The Lake Iroquois Association (LIA) was founded in 2007 to enhance the water quality of Lake Iroquois and to protect the health of the surrounding ecosystem.

Geographic entities mentioned:
surface_form: lake iroquois
instance_of: Lake
countries: United States
coordinates: lat: 40.5291
lon: -88.0932
surface_form: lake iroquois
instance_of: Lake
countries: United States
coordinates: lat: 40.5291
lon: -88.0932
surface_form: lake iroquois
instance_of: Lake
countries: United States
coordinates: lat: 44.3708
lon: -73.0844
surface_form: lake iroquois
instance_of: Lake
countries: United States
coordinates: lat: 44.3708
lon: -73.0844
surface_form: lake iroquois
instance_of: Lake
countries: United States
coordinates: lat: 44.34916667
lon: -97.83222222
surface_form: lake iroquois
instance_of: Lake
countries: United States
coordinates: lat: 44.34916667
lon: -97.83222222
In particular, the Yedisans are mentioned as a distinct group, and in various locations. Society. There were two groups of Nogais: those north of the Caspian Sea under their own Bey (leader), and those north of the Black Sea nominally subject to the Crimean Khan. The first group was broken up circa 1632 by the Kalmyks. The second shared the fate of the Khanate of Crimea.

Geographic entities mentioned:
surface_form: Caspian Sea
instance_of: Body of water
Lake
countries: Iran
Russia
Kazakhstan
Azerbaijan
Turkmenistan
Russian Empire
Soviet Union
coordinates: lat: 42
lon: 50.5
Quamichan Lake. Quamichan Lake is a lake in the Cowichan Valley region of Vancouver Island, British Columbia, Canada, located three kilometres to the northeast of the City of Duncan. Quamichan Lake and its sister Somenos Lake were created 11,000 years ago by receding glaciers. Both lakes contribute to Cowichan River.

Geographic entities mentioned:
surface_form: Somenos Lake
instance_of: Lake
countries: Canada
coordinates: lat: 48.80083
lon: -123.70278
surface_form: quamichan lake
instance_of: Lake
countries: Canada
coordinates: lat: 48.80139
lon: -123.66056
Quamichan Lake. Quamichan Lake is a lake in the Cowichan Valley region of Vancouver Island, British Columbia, Canada, located three kilometres to the northeast of the City of Duncan. Quamichan Lake and its sister Somenos Lake were created 11,000 years ago by receding glaciers. Both lakes contribute to Cowichan River.

Geographic entities mentioned:
surface_form: quamichan lake
instance_of: Lake
countries: Canada
coordinates: lat: 48.80139
lon: -123.66056
Quamichan Lake. Quamichan Lake is a lake in the Cowichan Valley region of Vancouver Island, British Columbia, Canada, located three kilometres to the northeast of the City of Duncan. Quamichan Lake and its sister Somenos Lake were created 11,000 years ago by receding glaciers. Both lakes contribute to Cowichan River.

Geographic entities mentioned:
surface_form: quamichan lake
instance_of: Lake
countries: Canada
coordinates: lat: 48.80139
lon: -123.66056
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
Quamichan Lake and its sister Somenos Lake were created 11,000 years ago by receding glaciers. Both lakes contribute to Cowichan River. Quamichan Lake's outflow is Quamichan Creek which joins with Somenos Creek, the outflow from Somenos Lake, which flows to Cowichan River. In autumn 2016, the lake's algae received public attention after news coverage of its killing at least four dogs. Name origin.

Geographic entities mentioned:
surface_form: quamichan lake
instance_of: Lake
countries: Canada
coordinates: lat: 48.80139
lon: -123.66056
Their community was adjacent to the lake. Habitat. The surface area of Quamichan Lake is with a maximum depth of and a mean depth of. The surrounding watershed for this large, shallow lake is. The Cowichan Garry Oak Preserve is located alongside the lake. The lake is habitat to algae and trout. There are also Pumpkinseed (invasive sunfish) and catfish in the lake.

Geographic entities mentioned:
surface_form: quamichan lake
instance_of: Lake
countries: Canada
coordinates: lat: 48.80139
lon: -123.66056
Many migratory birds winter in the lake as it rarely freezes over in the winter. In 2007 the Quamichan Watershed Stewardship Society (&quot;Quamichan Stewards&quot;) was formed by residents and farmers living around Quamichan Lake who were concerned about its degrading condition. Between 2010 and 2014, about 65,500 trout were added to the lake by a hatchery.

Geographic entities mentioned:
surface_form: quamichan lake
instance_of: Lake
countries: Canada
coordinates: lat: 48.80139
lon: -123.66056
He learns about a legendary custom shark, believed to be the spirit of a dead man who preys on white flesh. In Ambrym, known for its fire magic, he hears of ancient burial practices where chiefs' bones were kept in their homes to maintain their mana (spiritual power). He also meets Melanesians who retain connections to their ancestral religions despite missionary influences.

Geographic entities mentioned:
surface_form: Ambrym
instance_of: Mountain
countries: Vanuatu
coordinates: lat: -16.333333333333
lon: 168.33333333333
Batabat. Batabat (&quot;Azerbaijani:&quot; Batabat) is a tarn in the South Caucasus. It is located in Azerbaijan, in the mountains of Shahbuz District, Nakhichivan Autonomous Republic. Located at an elevation of 2,500 meters above sea level. There is a lake with a 16 ha area is remarkable with a peaty island floating on the surface of the water.

Geographic entities mentioned:
surface_form: batabat
instance_of: Lake
countries: Azerbaijan
coordinates: lat: 39.539166666667
lon: 45.784444444444
Batabat. Batabat (&quot;Azerbaijani:&quot; Batabat) is a tarn in the South Caucasus. It is located in Azerbaijan, in the mountains of Shahbuz District, Nakhichivan Autonomous Republic. Located at an elevation of 2,500 meters above sea level. There is a lake with a 16 ha area is remarkable with a peaty island floating on the surface of the water.

Geographic entities mentioned:
surface_form: batabat
instance_of: Lake
countries: Azerbaijan
coordinates: lat: 39.539166666667
lon: 45.784444444444
surface_form: batabat
instance_of: Lake
countries: Azerbaijan
coordinates: lat: 39.539166666667
lon: 45.784444444444
Units of the system can only be established by an act of the General Assembly of North Carolina. The park system began in 1916 when the summit of Mount Mitchell became first state park in the Southeastern United States.

Geographic entities mentioned:
surface_form: Mount Mitchell
instance_of: Mountain
countries: United States
coordinates: lat: 35.764722222222
lon: -82.265277777778
In all, 41 people were killed during the flooding events: 39 in Kentucky on July 28 and 2 in Missouri on July 26. More flooding events continued throughout August, impacting areas such as Death Valley, the Dallas–Fort Worth metroplex, and central Mississippi. A flash flood in Zion National Park in Utah led to one fatality.

Geographic entities mentioned:
surface_form: Death Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.45693888888889
lon: -116.86528055555556
Fugitive Slave Acts. Most escaped slaves, reaching Canada by boat across Lake Erie and Lake Ontario, settled in Ontario. More than 30,000 people were said to have escaped there via the network during its 20-year peak period, although U.S. Census figures account for only 6,000. Klondike Gold Rush.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
Montreux–Lenk im Simmental line. The Montreux–Lenk im Simmental line is a metre-gauge electric railway line in Switzerland run by the Montreux Oberland Bernois Railway (MOB) and links Montreux on Lake Geneva by way of Les Avants, Montbovon, Rossinière, Château-d'Œx, Rougemont, Saanen, Gstaad and Zweisimmen with Lenk im Simmental. It leads through the cantons of Vaud, Fribourg and Bern.

Geographic entities mentioned:
surface_form: Lake Geneva
instance_of: Lake
countries: Switzerland
France
coordinates: lat: 46.45
lon: 6.55
Description. Mt. Forddred is part of the Skagit Range which is a subrange of the North Cascades. It is situated southeast of Hope and north of Mount Payne which is the nearest higher neighbor. Precipitation runoff from the peak's west slope drains to the Fraser River via Silverhope Creek, whereas the north and east slopes drain into the Sumallo River.

Geographic entities mentioned:
surface_form: Mount Payne
instance_of: Mountain
countries: Canada
coordinates: lat: 49.1681
lon: -121.2883
Mount Forddred. Mount Forddred is a mountain summit located in the Canadian Cascades of British Columbia, Canada. Description. Mt. Forddred is part of the Skagit Range which is a subrange of the North Cascades. It is situated southeast of Hope and north of Mount Payne which is the nearest higher neighbor.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: mount forddred
instance_of: Mountain
countries: Canada
coordinates: lat: 49.203
lon: -121.2875
Topographic relief is significant as the summit rises 1,585 metres (5,200 feet) above Silverhope Creek in five kilometres (3.1 miles) and 1,128 metres (3,700 feet) above the Sumallo in three kilometres (1.86 mile). The mountain's toponym was officially adopted on April 7, 1955, by the Geographical Names Board of Canada.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Mount Forddred. Mount Forddred is a mountain summit located in the Canadian Cascades of British Columbia, Canada. Description. Mt. Forddred is part of the Skagit Range which is a subrange of the North Cascades. It is situated southeast of Hope and north of Mount Payne which is the nearest higher neighbor.

Geographic entities mentioned:
surface_form: mount forddred
instance_of: Mountain
countries: Canada
coordinates: lat: 49.203
lon: -121.2875
Winter temperatures can drop below −10 °C with wind chill factors below −20 °C. During winter months, weather is usually cloudy, but due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. The months of July through September offer the most favorable weather for viewing and climbing Mount Forddred. Geology.

Geographic entities mentioned:
surface_form: mount forddred
instance_of: Mountain
countries: Canada
coordinates: lat: 49.203
lon: -121.2875
Although no time frame is given, it is likely that sixty-nine-year-old Krapp's memories of being &quot;again in the dingle at Christmas Eve, gathering holly... [or] on Croghan on a Sunday morning, in the haze, with the bitch&quot; alludes to Beckett's own childhood familial memories. His birth-sign in early drafts is given as Aries, Beckett's own.

Geographic entities mentioned:
surface_form: Croghan
instance_of: Mountain
countries: Ireland
coordinates: lat: 52.8
lon: -6.3166666666667
Sava on his visit to the Holy Land. He was highly respected by both the royal court and the monks of Mount Athos. The Athonite scribe Teodore's account of his troubles, recorded on the pages of the &quot;Hexameron&quot; (&quot;Šestodnev&quot;) of John the Exarch, which Teodore copied at Domentijan's request, contains many references to Domentijan's humanity and the help he gave him.

Geographic entities mentioned:
surface_form: Mount Athos
instance_of: Mountain
countries: Greece
coordinates: lat: 40.15833333333333
lon: 24.327222222222222
The CHCH tower ranked thirteenth in height among the tallest structures in the Commonwealth of Nations. The mast was located on the edge of the Niagara Escarpment, so when viewed from the bottom of the escarpment with an elevation some 100+ meters or 300+ feet lower, it appeared exceptionally tall.

Geographic entities mentioned:
surface_form: Niagara Escarpment
instance_of: Mountain
countries: Canada
coordinates: lat: 43.8334
lon: -79.99966
Monumento del Llano Amarillo. Monumento del Llano Amarillo is a monument in the Spanish territory of Ceuta, in the North of Africa, at the bottom of Mount Hacho. The fifteen metre monument was moved here from Morocco in 1962 and it is one of the few sculptures left that record Spain's period of Nationalism following the Spanish Civil War. History.

Geographic entities mentioned:
surface_form: Mount Hacho
instance_of: Mountain
countries: Spain
coordinates: lat: 35.8969252
lon: -5.2867421
The same year he used &quot;Ajax&quot;s guns to bombard the breaches of the Spanish fortress town of San Sebastian during the British siege. In 1814, Otway convoyed merchant ships to Quebec and whilst in Canada was dispatched as a rear-admiral on a special commission to prepare the small ships squadron on Lake Champlain.

Geographic entities mentioned:
surface_form: Lake Champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
Its summit is a tripoint at which the borders of the municipalities of Miazzina, Aurano and Valle Cannobina meet. Along with Cima della Laurasca is the highest summit of the surrounding area. On the summit, which offers a very wide view on the surrounding mountain, stands a cross bearing a box sheltering a summit register. Access to the summit.

Geographic entities mentioned:
surface_form: Cima della Laurasca
instance_of: Mountain
countries: Italy
coordinates: lat: 46.0603
lon: 8.48376
surface_form: laurasca
instance_of: Mountain
countries: Italy
coordinates: lat: 46.0603
lon: 8.48376
Monte Zeda. The Monte Zeda is a mountain in the Lepontine Alps belonging to the Province of Verbano-Cusio-Ossola (Italy). Geography. The mountain is located in Piedmont (Provincia del Verbano-Cusio-Ossola), between two Alpine valleys: Val Grande and Val Cannobina. Its summit is a tripoint at which the borders of the municipalities of Miazzina, Aurano and Valle Cannobina meet.

Geographic entities mentioned:
surface_form: ossola
instance_of: Valley
countries: Italy
coordinates: lat: 46.283333333333
lon: 8.35
surface_form: monte zeda
instance_of: Mountain
countries: Italy
coordinates: lat: 46.04498
lon: 8.53576
surface_form: zeda
instance_of: Mountain
countries: Italy
coordinates: lat: 46.04498
lon: 8.53576
surface_form: cusio
instance_of: Lake
countries: Italy
coordinates: lat: 45.8098
lon: 8.3963
Monte Zeda. The Monte Zeda is a mountain in the Lepontine Alps belonging to the Province of Verbano-Cusio-Ossola (Italy). Geography. The mountain is located in Piedmont (Provincia del Verbano-Cusio-Ossola), between two Alpine valleys: Val Grande and Val Cannobina. Its summit is a tripoint at which the borders of the municipalities of Miazzina, Aurano and Valle Cannobina meet.

Geographic entities mentioned:
surface_form: ossola
instance_of: Valley
countries: Italy
coordinates: lat: 46.283333333333
lon: 8.35
surface_form: cusio
instance_of: Lake
countries: Italy
coordinates: lat: 45.8098
lon: 8.3963
Monte Zeda. The Monte Zeda is a mountain in the Lepontine Alps belonging to the Province of Verbano-Cusio-Ossola (Italy). Geography. The mountain is located in Piedmont (Provincia del Verbano-Cusio-Ossola), between two Alpine valleys: Val Grande and Val Cannobina. Its summit is a tripoint at which the borders of the municipalities of Miazzina, Aurano and Valle Cannobina meet.

Geographic entities mentioned:
surface_form: monte zeda
instance_of: Mountain
countries: Italy
coordinates: lat: 46.04498
lon: 8.53576
surface_form: zeda
instance_of: Mountain
countries: Italy
coordinates: lat: 46.04498
lon: 8.53576
On the summit, which offers a very wide view on the surrounding mountain, stands a cross bearing a box sheltering a summit register. Access to the summit. Reaching the summit of Monte Zeda does not require alpinistic skill. It can be accessed starting from Premeno through Alpe Manegra, Piancavallo and, later, &quot;Passo Folungo&quot; (a mountain pass at 1,369 m) and Alpe Archia.

Geographic entities mentioned:
surface_form: monte zeda
instance_of: Mountain
countries: Italy
coordinates: lat: 46.04498
lon: 8.53576
surface_form: zeda
instance_of: Mountain
countries: Italy
coordinates: lat: 46.04498
lon: 8.53576
Access to the summit. Reaching the summit of Monte Zeda does not require alpinistic skill. It can be accessed starting from Premeno through Alpe Manegra, Piancavallo and, later, &quot;Passo Folungo&quot; (a mountain pass at 1,369 m) and Alpe Archia. Another route to Monte Zeda starts from Falmenta and takes about 5 hours walking. Nature conservation.

Geographic entities mentioned:
surface_form: monte zeda
instance_of: Mountain
countries: Italy
coordinates: lat: 46.04498
lon: 8.53576
surface_form: zeda
instance_of: Mountain
countries: Italy
coordinates: lat: 46.04498
lon: 8.53576
It is the location of Marsden Point Oil Refinery and the Northport cargo port. Geography. The point is a broad, flat barrier spit, a peninsula of sand dunes, alluvium and estuarine deposits, that forms the southern head of the Whangārei Harbour entrance. It is southeast of Whangārei and around from Auckland's CBD.

Geographic entities mentioned:
surface_form: Mount Manaia
instance_of: Mountain
countries: New Zealand
coordinates: lat: -35.818309
lon: 174.516985
A regional journal on ethnology, &quot;Le Monde alpin et rhodanien&quot; published two to four issues per year from 1973 to 2006. It featured studies and articles on Southeastern France, especially on important geographical landmarks such as the Alps, the Rhône, the historical Lyonnais province, the Po Valley, Lake Geneva, and the Camargue region.

Geographic entities mentioned:
surface_form: Po Valley
instance_of: Valley
countries: Italy
coordinates: lat: 45.330277777778
lon: 9.7988888888889
surface_form: Lake Geneva
instance_of: Lake
countries: Switzerland
France
coordinates: lat: 46.45
lon: 6.55
Fee Glacier. The Fee Glacier () is a long glacier (2005) situated in the Pennine Alps in the canton of Valais in Switzerland. In 1973, it had a length of and an area of. It lies east of the Mischabel range, between the summit of Dom on the north and Allalinhorn on the south. The glacier is accessible via the Mittelallalin cable car and is used as a ski area. Physical characteristics.

Geographic entities mentioned:
surface_form: Allalinhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.046138888889
lon: 7.8948055555556
Fee Glacier. The Fee Glacier () is a long glacier (2005) situated in the Pennine Alps in the canton of Valais in Switzerland. In 1973, it had a length of and an area of. It lies east of the Mischabel range, between the summit of Dom on the north and Allalinhorn on the south. The glacier is accessible via the Mittelallalin cable car and is used as a ski area. Physical characteristics.

Geographic entities mentioned:
surface_form: Mittelallalin
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.057672222222
lon: 7.9049666666667
division. Chapman left the company in 1999. He currently owns many properties and companies throughout the United States, including the Brooks Lake Lodge, a private 800-acre ranch in Dubois, WY and the Snow King Mountain Resort which has the one-of-a-kind Snow King Observatory and Planetarium in Jackson Hole, Wyoming. Philanthropy.

Geographic entities mentioned:
surface_form: Jackson Hole
instance_of: Valley
countries: United States
coordinates: lat: 43.516666666667
lon: -110.83333333333
Egge, Innlandet. Egge is a village in Gran Municipality in Innlandet county, Norway. The village is located about to the northwest of the village of Brandbu. The lake Randsfjorden and the Nes Church are both about to the east of Egge.

Geographic entities mentioned:
surface_form: Randsfjorden
instance_of: Lake
countries: Norway
coordinates: lat: 60.390277777778
lon: 10.394166666667
Monte Summano. Monte Summano is a mountain in the Veneto region, Italy. It has an elevation of 1,296 metres.

Geographic entities mentioned:
surface_form: monte summano
instance_of: Mountain
countries: Italy
coordinates: lat: 45.75972222
lon: 11.39
Pirdop Gate on Livingston Island in the South Shetland Islands, Antarctica is named after Pirdop. Geography. The town is situated in the Zlatitsa–Pirdop Valley, the highest of the eleven Sub-Balkan valleys at an altitude of 670 m. It is surrounded by the Balkan Mountains to the north, the Sredna Gora mountain range to the south, and Koznitsa and Galabets saddles to the east and west, respectively.

Geographic entities mentioned:
surface_form: Sub-Balkan valleys
instance_of: Valley
countries: Bulgaria
coordinates: lat: 42.616666666667
lon: 24.716666666667
Dudleya verityi. &quot;Dudleya verityi&quot; is a rare species of succulent plant known by the common name Verity's liveforever. It is endemic to Ventura County, California, where it is known from only three occurrences in the vicinity of Conejo Mountain between Camarillo and Thousand Oaks. It probably occurs in a few additional locations nearby which have not yet been officially vouchered.

Geographic entities mentioned:
surface_form: Conejo Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 34.18833333
lon: -118.98444444
It is named after Sir David Brewster (1781–1868) who described it in 1822. The type locality for the series and for brewsterite-Sr is Strontian, Argyll, Scotland. It is a hydrothermal mineral occurring in volcanic rocks such as basalt. Grayish crystals are found at the Giant's Causeway in County Antrim. It is found with harmotome in the lead mines at Strontian in Argyllshire.

Geographic entities mentioned:
surface_form: Giant's Causeway
instance_of: Landform
countries: United Kingdom
coordinates: lat: 55.240833333333
lon: -6.5116666666667
Namesakes. Ezekiel Bishop Hart was born c. 1795. He entered the Navy as a Midshipman on 30 April 1814. He was killed in the action of Commodore Isaac Chauncey's squadron on Lake Ontario on 26 August 1814. John E. Hart was appointed a Midshipman on 23 February 1841. He served on various ships of the fleet, and was appointed Lieutenant Commander in July 1862.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
It is the only crocodile species capable of living in both saltwater and freshwater environments and is native to the entire Southeast Asian archipelago, ranging from the eastern coast of India to the northern coast of Australia. In East Timor, a population of approximately 300 saltwater crocodiles resides in isolation at Ira Lalaro, the country's largest lake, and its connected rivers.

Geographic entities mentioned:
surface_form: Ira Lalaro
instance_of: Lake
countries: Timor-Leste
coordinates: lat: -8.45
lon: 127.133
These crocodiles exclusively inhabit freshwater environments, located about nine kilometers inland from the sea. They are geographically separated from the coast by the Paitchau mountain range, preventing contact with the ocean or other populations of their species. Crocodile in East Timor. The crocodile is a national symbol of East Timor.

Geographic entities mentioned:
surface_form: Paitchau
instance_of: Mountain
countries: Timor-Leste
coordinates: lat: -8.50472222
lon: 127.16444444
Lapland Biosphere Reserve. Lapland Nature Reserve () (also Laplandskiy) is a Russian &quot;zapovednik&quot; (strict nature reserve) in Murmansk Oblast, Russia, above the Arctic Circle. Officially established in 1957, the reserve protects an area of to the northwest of Lake Imandra, including 86 km² of inland water. The terrain is mountainous tundra and northern taiga.

Geographic entities mentioned:
surface_form: Lake Imandra
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.5542
lon: 33.0484
Wila Pukara (Aroma). Wila Pukara (Aymara &quot;wila&quot; blood, blood-red, &quot;pukara&quot; fortress, &quot;red fortress&quot;, also spelled &quot;Wila Pucara&quot;) is a mountain in the Bolivian Andes which reaches a height of approximately. It is located in the La Paz Department, Aroma Province, Sica Sica Municipality.

Geographic entities mentioned:
surface_form: pukara
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.7944
lon: -68.9267
surface_form: pukara
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.95138931
lon: -67.91166687
surface_form: wila pukara (aroma)
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.28861111
lon: -67.69166667
surface_form: pukara
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.72972222
lon: -65.88138889
surface_form: wila pukara
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.135
lon: -67.4472
surface_form: pukara
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.6136
lon: -68.7567
surface_form: pukara
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.30416667
lon: -66.95361111
surface_form: pukara
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.28472222
lon: -67.985
surface_form: pukara
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.73888889
lon: -65.78333333
surface_form: pukara
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.95833333
lon: -68.01388889
surface_form: pukara
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.7261
lon: -68.5892
surface_form: pukara
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.86055556
lon: -68.65444444
surface_form: pukara
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.87416667
lon: -68.21083333
surface_form: pukara
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.9394
lon: -68.5722
surface_form: pukara
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.86444444
lon: -68.10694444
In terms of the number of events related to the cultures of the Quechua and Aymara peoples and of the mestizos of the Altiplano, and also in terms of the number of people directly and indirectly involved in its realization, it stands with the Carnival in Rio de Janeiro and the Carnaval de Oruro in Bolivia as one of the three largest festivals in South America.

Geographic entities mentioned:
surface_form: Altiplano
instance_of: Plateau
countries: Bolivia
Peru
Chile
Argentina
coordinates: lat: -16.00358
lon: -69.65332
Aged only 18 he was appointed lecturer at Hamburg University, Germany and afterwards left for England. He migrated to Australia, working variously as surveyor on the Mount Bischoff railway, Tasmania and the Nyngan-Byrock railway, interspersed with botanical collecting in Qld.

Geographic entities mentioned:
surface_form: Mount Bischoff
instance_of: Mountain
countries: Australia
coordinates: lat: -41.416666666667
lon: 145.51666666667
The Marching Men is located in Arches National Park in the remote northwest section that was added to the park in 1971 when the boundaries of Arches National Monument were expanded and the monument changed to National Park status. Unofficial names for some of the seven towers include Cuddlebunny Tower, Time Tower, and North Marcher, although the National Park Service does acknowledge these names.

Geographic entities mentioned:
surface_form: seven
instance_of: Mountain
coordinates: lat: -69.6833
lon: 64.7
surface_form: park
instance_of: Mountain
coordinates: lat: -67.2333
lon: 51
Marching Men (Utah). Marching Men is an area of pillars in Grand County, Utah, United States. Description. The Marching Men is located in Arches National Park in the remote northwest section that was added to the park in 1971 when the boundaries of Arches National Monument were expanded and the monument changed to National Park status.

Geographic entities mentioned:
surface_form: park
instance_of: Mountain
coordinates: lat: -67.2333
lon: 51
surface_form: park
instance_of: Mountain
coordinates: lat: -67.2333
lon: 51
surface_form: park
instance_of: Mountain
coordinates: lat: -67.2333
lon: 51
surface_form: marching men
instance_of: Mountain
coordinates: lat: 38.7858105
lon: -109.6676211
Climate. According to the Köppen climate classification system, Marching Men is located in a cold semi-arid climate zone with cold winters and hot summers. Spring and fall are the most favorable seasons to experience Arches National Park, when highs average and lows average. Summer temperatures often exceed. Winters are cold, with highs averaging, and lows averaging.

Geographic entities mentioned:
surface_form: park
instance_of: Mountain
coordinates: lat: -67.2333
lon: 51
Winters are cold, with highs averaging, and lows averaging. As part of a high desert region, it can experience wide daily temperature fluctuations. The park receives an average of less than 10 inches (25 cm) of rain annually. Geology. Like most of the arches and rock formations in the park, these spires are composed of Entrada Sandstone, specifically the Slick Rock Member.

Geographic entities mentioned:
surface_form: park
instance_of: Mountain
coordinates: lat: -67.2333
lon: 51
Geology. Like most of the arches and rock formations in the park, these spires are composed of Entrada Sandstone, specifically the Slick Rock Member. Because the sandstone is not uniformly cemented with calcium carbonate which is the binding material, chemical weathering and differential erosion has sculpted the iconic landforms of Arches National Park.

Geographic entities mentioned:
surface_form: park
instance_of: Mountain
coordinates: lat: -67.2333
lon: 51
This landform's descriptive toponym has been officially adopted by the United States Board on Geographic Names. Climbing. The first ascent of the highest tower, North Marcher, was made by Leonard Coyne, Dennis Jackson, and Stewart Green in November 1979. Rock climbing at Marching Men is strictly regulated, including temporary closure from March 1 through August 31 for raptor protection. Climate.

Geographic entities mentioned:
surface_form: jackson
instance_of: Mountain
coordinates: lat: -71.3833
lon: -63.3667
Marching Men (Utah). Marching Men is an area of pillars in Grand County, Utah, United States. Description. The Marching Men is located in Arches National Park in the remote northwest section that was added to the park in 1971 when the boundaries of Arches National Monument were expanded and the monument changed to National Park status.

Geographic entities mentioned:
surface_form: marching men
instance_of: Mountain
coordinates: lat: 38.7858105
lon: -109.6676211
Topographic relief is modest as the summit of the highest, North Marcher, rises above surrounding terrain in laterally. Any scant precipitation runoff from Marching Men drains to the nearby Colorado River via Klondike Wash and Salt Valley Wash. The Marching Men area is accessed by a six-mile loop hike that starts at the Klondike Bluffs parking area, and also leads to Tower Arch.

Geographic entities mentioned:
surface_form: marching men
instance_of: Mountain
coordinates: lat: 38.7858105
lon: -109.6676211
Any scant precipitation runoff from Marching Men drains to the nearby Colorado River via Klondike Wash and Salt Valley Wash. The Marching Men area is accessed by a six-mile loop hike that starts at the Klondike Bluffs parking area, and also leads to Tower Arch. This landform's descriptive toponym has been officially adopted by the United States Board on Geographic Names. Climbing.

Geographic entities mentioned:
surface_form: marching men
instance_of: Mountain
coordinates: lat: 38.7858105
lon: -109.6676211
This landform's descriptive toponym has been officially adopted by the United States Board on Geographic Names. Climbing. The first ascent of the highest tower, North Marcher, was made by Leonard Coyne, Dennis Jackson, and Stewart Green in November 1979. Rock climbing at Marching Men is strictly regulated, including temporary closure from March 1 through August 31 for raptor protection. Climate.

Geographic entities mentioned:
surface_form: marching men
instance_of: Mountain
coordinates: lat: 38.7858105
lon: -109.6676211
Climate. According to the Köppen climate classification system, Marching Men is located in a cold semi-arid climate zone with cold winters and hot summers. Spring and fall are the most favorable seasons to experience Arches National Park, when highs average and lows average. Summer temperatures often exceed. Winters are cold, with highs averaging, and lows averaging.

Geographic entities mentioned:
surface_form: marching men
instance_of: Mountain
coordinates: lat: 38.7858105
lon: -109.6676211
These towers are the result of erosion and weathering that reduced vertical cross joints of a fin to rock pinnacles. The Marching Men terrain is similar to that of the Devils Garden area to the east, but the two areas are separated by the flat expanse of Salt Valley which was created by a collapsed salt anticline.

Geographic entities mentioned:
surface_form: marching men
instance_of: Mountain
coordinates: lat: 38.7858105
lon: -109.6676211
Hank finishes Ashby's biography. Charlie ends up working at a BMW dealership in the Valley, introducing himself as Chuck Runkle. Sonja's baby arrives; it is biracial, which proves that Hank cannot be the father. Hank and Karen slowly move toward reuniting. Karen is offered a job in New York, and Hank is happy to go there with her.

Geographic entities mentioned:
surface_form: the Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
Tschuggen (Wengen). The Tschuggen is a mountain of the Bernese Alps, overlooking Wengen in the Bernese Oberland. It has an elevation of 2,521 metres above sea level and it is the highest summit of the group lying north of the Kleine Scheidegg.

Geographic entities mentioned:
surface_form: tschuggen
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.783333333333
lon: 9.6644444444444
surface_form: tschuggen
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.6003
lon: 7.9495