Sarmila/GeoWiki-Features huggingface dataset:
On arrival, Jogues wrote to his mother: &quot;I do not know it is to enter Heaven, but this I know—that it would be difficult to experience in this world a joy more excessive and more overflowing than I felt in setting foot in the New World, and celebrating my first Mass on the day of Visitation.&quot;
Jogues joined Jean de Brébeuf, the superior of the Jesuit mission, at their settlement on Lake Huron, the village of St-Joseph (Ihonatiria), on 11 September.

Geographic entities mentioned:
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
There is also the Martyr's Shrine located in Midland, Ontario, Canada, which honors the Canadian Martyrs (another term for the North American Martyrs). A seasonal chapel on the east shore of Saratoga Lake, New York is named after Jogues. A statue of Jogues stands in front of the main entrance to the chapel that faces the lake.

Geographic entities mentioned:
surface_form: Saratoga Lake
instance_of: Lake
countries: United States
coordinates: lat: 43.02
lon: -73.74
Precipitation runoff from the peak drains north to Downton Lake which is a reservoir of the Bridge River. Mount Sloan is more notable for its steep rise above local terrain than for its absolute elevation as topographic relief is significant with the summit rising over 1,960 meters (6,430 ft) above Downton Lake in. Mount Penrose rises to the north on the opposite side of the lake. Etymology.

Geographic entities mentioned:
surface_form: Mount Penrose
instance_of: Mountain
countries: Canada
coordinates: lat: 50.8703
lon: -122.96
Description. Mount Sloan is the sixth-highest peak in the Thiassi Range which is a subrange of the Coast Mountains. The remote mountain is situated north of Pemberton and west of the historic gold-mining community of Bralorne. Precipitation runoff from the peak drains north to Downton Lake which is a reservoir of the Bridge River.

Geographic entities mentioned:
surface_form: remote mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4664
lon: -125.51975
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Mount Sloan. Mount Sloan is a mountain summit located in British Columbia, Canada. Description. Mount Sloan is the sixth-highest peak in the Thiassi Range which is a subrange of the Coast Mountains. The remote mountain is situated north of Pemberton and west of the historic gold-mining community of Bralorne.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: mount sloan
instance_of: Mountain
countries: Canada
coordinates: lat: 50.78194444444444
lon: -122.97166666666666
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Mount Sloan. Mount Sloan is a mountain summit located in British Columbia, Canada. Description. Mount Sloan is the sixth-highest peak in the Thiassi Range which is a subrange of the Coast Mountains. The remote mountain is situated north of Pemberton and west of the historic gold-mining community of Bralorne.

Geographic entities mentioned:
surface_form: mount sloan
instance_of: Mountain
countries: Canada
coordinates: lat: 50.78194444444444
lon: -122.97166666666666
Precipitation runoff from the peak drains north to Downton Lake which is a reservoir of the Bridge River. Mount Sloan is more notable for its steep rise above local terrain than for its absolute elevation as topographic relief is significant with the summit rising over 1,960 meters (6,430 ft) above Downton Lake in. Mount Penrose rises to the north on the opposite side of the lake. Etymology.

Geographic entities mentioned:
surface_form: mount sloan
instance_of: Mountain
countries: Canada
coordinates: lat: 50.78194444444444
lon: -122.97166666666666
Climate. Based on the Köppen climate classification, Mount Sloan is located in a subarctic climate zone of western North America. Most weather fronts originate in the Pacific Ocean, and travel east toward the Coast Mountains where they are forced upward by the range (Orographic lift), causing them to drop their moisture in the form of rain or snowfall.

Geographic entities mentioned:
surface_form: mount sloan
instance_of: Mountain
countries: Canada
coordinates: lat: 50.78194444444444
lon: -122.97166666666666
Mount Penrose rises to the north on the opposite side of the lake. Etymology. The mountain was presumably named after David Sloan who was a mining engineer and managing director at the Pioneer Mine just east of Bralorne. He died on August 4, 1935, from injuries received in a floatplane crash at Alta Lake on July 30, 1935. The crash also took the lives of the pilot, William R.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
The crash also took the lives of the pilot, William R. McCluskey, Reginald Walter Brock and his wife Mildred. The mountain's toponym was officially adopted September 6, 1951, by the Geographical Names Board of Canada. Climate. Based on the Köppen climate classification, Mount Sloan is located in a subarctic climate zone of western North America.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Etymology. The mountain was presumably named after David Sloan who was a mining engineer and managing director at the Pioneer Mine just east of Bralorne. He died on August 4, 1935, from injuries received in a floatplane crash at Alta Lake on July 30, 1935. The crash also took the lives of the pilot, William R. McCluskey, Reginald Walter Brock and his wife Mildred.

Geographic entities mentioned:
surface_form: alta lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.11472222222222
lon: -122.98194444444445
In addition to this, Trengrouse was dismayed at the then common practice of burying victims of shipwrecks in common graves in unconsecrated ground near the site of the wreck, having seen the dead from the &quot;Anson&quot; buried in the dunes at Loe Bar. He persuaded his local MP, Davies Gilbert, to work for a change in the law, and from 1808 the practice was abolished. Early life.

Geographic entities mentioned:
surface_form: Loe Bar
instance_of: Lake
countries: United Kingdom
coordinates: lat: 50.0764
lon: -5.28944
The red sandstone found throughout Red Rocks Park is geologically identified as belonging to the Fountain Formation. Other Colorado examples of Fountain Formation geology include nearby Roxborough State Park, Garden of the Gods near Colorado Springs, and the Flatirons near Boulder.

Geographic entities mentioned:
surface_form: Flatirons
instance_of: Mountain
countries: United States
coordinates: lat: 39.9883
lon: -105.293
British Admiral Edward Belcher attended and described her funeral in detail. Her remains were later transported along with those of other royals in a midnight torchlight procession on October 30, 1865, to the newly constructed Mauna ʻAla Royal Mausoleum up in the Nuʻuanu Valley.

Geographic entities mentioned:
surface_form: Nuʻuanu Valley
instance_of: Landform
countries: United States
coordinates: lat: 21.370277777778
lon: -157.79694444444
Lawrence residents had originally proposed opening a private Free-State college in the town when it was first settled, in the summer of 1854. That fall, one of the agents of the New England Emigrant Aid Company, Charles Robinson, told treasurer Amos Adams Lawrence that the citizens of Lawrence would begin a college as soon as possible, to be located atop Hogback Ridge (later known as Mount Oread).

Geographic entities mentioned:
surface_form: Mount Oread
instance_of: Mountain
countries: United States
coordinates: lat: 38.9631
lon: -95.2571
If Lawrence failed to meet these conditions, Emporia instead of Lawrence would get the university. The site selected for the university was a hill known as Hogback Ridge or Mount Oread, which was owned by former Kansas Governor Charles L. Robinson. Robinson and his wife Sara traded the site to the State of Kansas in exchange for land elsewhere.

Geographic entities mentioned:
surface_form: Mount Oread
instance_of: Mountain
countries: United States
coordinates: lat: 38.9631
lon: -95.2571
Mount Utsugi. __NOTOC__
is a mountain located on the boundary of Okuwa, Iijima and Miyada, Nagano Prefecture, in the Chūbu region of Japan. It is tall and part of the Kiso Mountains. It is also included on the list of &quot;100 Famous Japanese Mountains.&quot;
Hiking. The landscape of Mt. Utsugi includes large granite boulders surrounded by lush greenery.

Geographic entities mentioned:
surface_form: mount utsugi
instance_of: Mountain
countries: Japan
coordinates: lat: 35.71888889
lon: 137.81694444
Location. Adirondack Woodcraft Summer Camps is located in the Adirondacks in upstate New York in Old Forge. The summer camp is located in Herkimer County in the Town of Webb and encompasses 250 acres surrounding two private lakes, Lake Kan-ac-to and Lake Te-jec-na, two small kettle lakes about four miles northeast of the village of Old Forge.

Geographic entities mentioned:
surface_form: Lake Kan-ac-to
instance_of: Lake
countries: United States
coordinates: lat: 43.7515286
lon: -74.9263608
surface_form: Lake Te-jec-na
instance_of: Lake
countries: United States
coordinates: lat: 43.753589
lon: -74.926037
Victory Boulevard (Los Angeles). Victory Boulevard is a major mostly east–west arterial road that runs for traversing almost the entire length of the San Fernando Valley in Los Angeles and Burbank, California. About of the boulevard runs north–south before reaching its eastern terminus. History. When Van Nuys was plotted in 1911, Victory Boulevard was called 7th Avenue.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
It is native to central Chile from 30 to 35°S., up to 1200 meters (4000 ft) above sea level and lives under very dry conditions. A type locality for &quot;B. miersii&quot; is the La Campana National Park and Cerro La Campana, where it is associated with the endangered Chilean wine palm. Description. Reaches 25 meters (82 ft) height and 80 cm (31 in) diameter. Straight and cylindrical trunk.

Geographic entities mentioned:
surface_form: Cerro La Campana
instance_of: Mountain
countries: Chile
coordinates: lat: -32.953611111111
lon: -71.119444444444
Political geography and history. Chilliwack was the successor riding to Westminster-Chilliwhack, which was one of four subdivisions of the old rural Westminster riding, the others being the ridings that became, after similar name-changes, Delta, Dewdney and Richmond, which are the parent ridings of all current Fraser Valley electoral districts. Chilliwack riding lasted until the 1996 election.

Geographic entities mentioned:
surface_form: Fraser Valley
instance_of: Valley
countries: Canada
coordinates: lat: 49.108333333333
lon: -122.29166666667
It is the highest point in the South Gondar Zone, with an elevation of above sea level. Mount Guna forms part of the divide between the drainage basins of the Abay and the Tekezé rivers. It is the origin of the Gumara, Rib, and other rivers, which flow into Lake Tana and Yikalo, Mebela, Goleye and other rivers, which flow into the Tekezé river.

Geographic entities mentioned:
surface_form: Lake Tana
instance_of: Lake
countries: Ethiopia
coordinates: lat: 12
lon: 37.25
surface_form: tana
instance_of: Lake
countries: Ethiopia
coordinates: lat: 12
lon: 37.25
surface_form: lake tana
instance_of: Lake
countries: Ethiopia
coordinates: lat: 12
lon: 37.25
Mount Guna. Mount Guna (Amharic: ጉና ተራራ, &quot;Guna Terara&quot;) is a mountain and shield volcano located near the cities of Nefas Mewcha and Debre Tabor, in the northern Amhara Region of Ethiopia. It is the highest point in the South Gondar Zone, with an elevation of above sea level. Mount Guna forms part of the divide between the drainage basins of the Abay and the Tekezé rivers.

Geographic entities mentioned:
surface_form: mount guna
instance_of: Mountain
countries: Ethiopia
coordinates: lat: 11.7108
lon: 38.2367
surface_form: guna
instance_of: Mountain
countries: Ethiopia
coordinates: lat: 11.7108
lon: 38.2367
Mount Guna. Mount Guna (Amharic: ጉና ተራራ, &quot;Guna Terara&quot;) is a mountain and shield volcano located near the cities of Nefas Mewcha and Debre Tabor, in the northern Amhara Region of Ethiopia. It is the highest point in the South Gondar Zone, with an elevation of above sea level. Mount Guna forms part of the divide between the drainage basins of the Abay and the Tekezé rivers.

Geographic entities mentioned:
surface_form: mount guna
instance_of: Mountain
countries: Ethiopia
coordinates: lat: 11.7108
lon: 38.2367
surface_form: guna
instance_of: Mountain
countries: Ethiopia
coordinates: lat: 11.7108
lon: 38.2367
surface_form: guna
instance_of: Mountain
countries: Ethiopia
coordinates: lat: 11.7108
lon: 38.2367
Geography. Montagnais of Natashquan owns one reserve, Nutashkuan located in the Côte-Nord region of Quebec close to the municipality of Natashquan. The reserve is at the mouth of the Natashquan River on the northern coast of the Gulf of St. Lawrence. It covers an area of. The reserve is east of Sept-Îles and east of Quebec City via Quebec Route 138. The band is also served by Natashquan Airport.

Geographic entities mentioned:
surface_form: Natashquan River
instance_of: Watercourse
countries: Canada
coordinates: lat: 50.118611
lon: -61.807222
The second order short mountain range adjoins the main ridge spurs of Kuznetsk Alatau. The length is from the southwest to the northeast. Kharatas branches off from the main ridge of the Kuznetsk Alatau in the region of Mount Verkhny Zub and is the watershed of the Kharatas and Bely Iyus rivers. Absolute heights increase from north to south, from to (mountain Staraya Krepost).

Geographic entities mentioned:
surface_form: Mount Verkhny Zub
instance_of: Mountain
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.838055555556
lon: 89.237222222222
Pukala. tr3sr9vneftnq4l7cvj7hi5ln04bx" xml:space="preserve">Pukālā (Nepalese language: पुकाला, &quot;fried meat&quot;) is a traditional dish of boiled and fried variety meats of the water buffalo. The dish is a delicacy in the Newar cuisine of the Kathmandu Valley in Nepal and is enjoyed during wedding and festival feasts. It is served after the main course and before dessert.

Geographic entities mentioned:
surface_form: Kathmandu Valley
instance_of: Valley
countries: Nepal
coordinates: lat: 27.703944444444
lon: 85.308583333333
Miyolangsangma. y8zlf4bxca54u7j870nr0zelsq9tu" xml:space="preserve">Miyolangsangma is the Tibetan Buddhist goddess who lives at the top of Chomolungma (Mount Everest). She is one of the five long-life sisters and her virtue is inexhaustible giving. She started out as a malevolent demoness and was converted by a great Buddhist.

Geographic entities mentioned:
surface_form: Mount Everest
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.988055555555555
lon: 86.925
It was founded in 1903 by the Cima brothers and closed its doors in 1968. The company &quot;CimaNorma S.A.&quot; also stands for the economic development and modernization advancement goal from the beginning of the 20th century for the mountain valley Blenio Valley, which was classified as a peripheral region.

Geographic entities mentioned:
surface_form: Blenio Valley
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.427563888889
lon: 8.9698222222222
CimaNorma manufactured all products related to cocoa; from chocolate powder to chocolate bars. The factory complex, still in existence today, is located at the entrance of the Val Soia, at the foot of the Rheinwaldhorn massif. A foundation promoting culture, La Fabbrica del Cioccolato, was established in 2016. It offers space in the former industrial complex for creators of contemporary art.

Geographic entities mentioned:
surface_form: Rheinwaldhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.493611111111
lon: 9.04
The sparsely populated Blenio Valley, traditionally characterized in the past by subsistence-oriented forestry, arable farming and pasture farming, by viticulture in small plots and by emigration, developed forms of seasonal emigration in the 18th century in which better-off families also remained involved: the mostly male emigrants moving with the seasons to the urban centers of Europe (Paris, Milan, Pavia, Turin, Genoa, Lyon, Nice, Frankfurt, Amsterdam etc.), where they sold sweets, such as chestnuts or chocolate.

Geographic entities mentioned:
surface_form: Blenio Valley
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.427563888889
lon: 8.9698222222222
This enabled the establishment of permanent sales outlets or cafes, restaurants and hotels and the accumulation of expertise and investment capital. The best-known example of such a success story is the curriculum vitae of the entrepreneur Carlo Gatti (1817–1878) from Dongio in the Blenio Valley, whose restaurants and ice cream production brought him great wealth in England.

Geographic entities mentioned:
surface_form: Blenio Valley
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.427563888889
lon: 8.9698222222222
But the novice architect also learned from working in the Boston office of Alexander Parris, whose characteristic work in granite influenced Young's subsequent governmental commissions. In 1830, Young opened his own office in Burlington, Vermont, a trade center growing fast since the 1823 opening of the Champlain Canal which connected Lake Champlain with the Hudson River and New York City.

Geographic entities mentioned:
surface_form: Lake Champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
From there, they reached a place called Barik near Fayzabad, Badakhshan. From there, they reached Chitral via Zebak where they received assistance from Mehtar Amir ul-Mulk, and subsequently went to Dargai. After months of walking on foot, they finally went from Dargai to Amritsar via rail.

Geographic entities mentioned:
surface_form: Chitral
instance_of: Valley
countries: Pakistan
coordinates: lat: 35.85111111111111
lon: 71.78888888888889
The force numbered 8,274 infantry, 1,618 cavalry, 32 cannon, and 8 howitzers. Davidovich fought at the Battle of Castiglione on 5 August. In the second relief of Mantua, Wurmser and his chief of staff Franz von Lauer planned to transfer major elements of the army from the upper Adige valley to Bassano del Grappa via the Valsugana.

Geographic entities mentioned:
surface_form: Valsugana
instance_of: Valley
countries: Italy
coordinates: lat: 46
lon: 11.666666666667
San José (volcano). San José Volcano is the stratovolcano that gives its name to a massive volcanic group, at about from Santiago de Chile at the end of the Cajón del Maipo on the Chile-Argentina border.

Geographic entities mentioned:
surface_form: Cajón del Maipo
instance_of: Valley
countries: Chile
coordinates: lat: -33.633333333333
lon: -70.35
surface_form: san josé
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -33.781666666667
lon: -69.897222222222
San José Volcano is the stratovolcano that gives its name to a massive volcanic group, at about from Santiago de Chile at the end of the Cajón del Maipo on the Chile-Argentina border. It lies on the south end of an approximately x complex that includes the La Engorda, Espiritu Santo, Plantat and Marmolejo volcanoes, the latter of which is located on the Northern end of the group.

Geographic entities mentioned:
surface_form: Marmolejo
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -33.717129
lon: -69.864514
San José (volcano). San José Volcano is the stratovolcano that gives its name to a massive volcanic group, at about from Santiago de Chile at the end of the Cajón del Maipo on the Chile-Argentina border.

Geographic entities mentioned:
surface_form: san josé
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -33.781666666667
lon: -69.897222222222
Rahajärvi. Rahajärvi (also: Raahajärvi) is a medium-sized lake in the Paatsjoki main catchment area. It is located in the municipality of Inari in the region Lapland in Finland. The lake has major and minor part. It is situated near the Finnish National Road 4.

Geographic entities mentioned:
surface_form: rahajärvi
instance_of: Lake
countries: Finland
coordinates: lat: 64.0055894
lon: 26.8240444
Rahajärvi. Rahajärvi (also: Raahajärvi) is a medium-sized lake in the Paatsjoki main catchment area. It is located in the municipality of Inari in the region Lapland in Finland. The lake has major and minor part. It is situated near the Finnish National Road 4.

Geographic entities mentioned:
surface_form: inari
instance_of: Lake
countries: Finland
coordinates: lat: 68.9596511
lon: 27.6017069
Wholdaia Lake. Wholdaia Lake is a lake in the Northwest Territories, Canada. It is drained northward by the Dubawnt River.

Geographic entities mentioned:
surface_form: wholdaia lake
instance_of: Lake
countries: Canada
coordinates: lat: 60.7168801
lon: -104.1672967
Kronberg (Lower Bavaria). Kronberg (Niederbayern) is a mountain of Bavaria, Germany.

Geographic entities mentioned:
surface_form: kronberg
instance_of: Mountain
countries: Germany
coordinates: lat: 49.037
lon: 13.1052
It stands immediately north of Sticks Pass on the main ridge of the Helvellyn range in the Eastern Fells, which is situated between the lakes of Thirlmere and the Ullswater. The summit of Stybarrow Dodd is a smooth, rounded, grassy dome, like those of its two northern neighbours, Watson's Dodd and Great Dodd. Together, these three rather similar fells are sometimes called ‘The Three Dodds’.

Geographic entities mentioned:
surface_form: Watson's Dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5672
lon: -3.02849
surface_form: Great Dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.575411111111
lon: -3.0194111111111
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
surface_form: stybarrow dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.56105
lon: -3.0175111111111
surface_form: watson's dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5672
lon: -3.02849
surface_form: great dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.575411111111
lon: -3.0194111111111
This ridge runs north–south for about without dropping below. Stybarrow Dodd occupies just over of this length, from Sticks Pass to the col which connects it to Watson's Dodd and Great Dodd. At this point the ridge is the watershed between the Eden river system to the east and the Derwent river system to the west. The fell rises to, standing nearly above Sticks Pass and above the col to the north.

Geographic entities mentioned:
surface_form: Watson's Dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5672
lon: -3.02849
surface_form: Great Dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.575411111111
lon: -3.0194111111111
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
surface_form: watson's dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5672
lon: -3.02849
surface_form: great dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.575411111111
lon: -3.0194111111111
All of these becks flow directly into Ullswater. There is more detail about each of these ridges and their subsidiary tops on the Hart Side and Sheffield Pike pages. There are also two short spurs to the north of the main summit. To the north-west one spur leads down to the col which connects the fell to Watson's Dodd and Great Dodd.

Geographic entities mentioned:
surface_form: Hart Side
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5693
lon: -2.99297
surface_form: Sheffield Pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.555080555556
lon: -2.9787
surface_form: sheffield pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.555080555556
lon: -2.9787
surface_form: hart side
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5693
lon: -2.99297
There are also two short spurs to the north of the main summit. To the north-west one spur leads down to the col which connects the fell to Watson's Dodd and Great Dodd. To the north-east a longer spur called Middle Tongue runs down into Deepdale, between Browndale Beck and Aira Beck. Sticks Pass.

Geographic entities mentioned:
surface_form: Watson's Dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5672
lon: -3.02849
surface_form: Great Dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.575411111111
lon: -3.0194111111111
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
surface_form: watson's dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5672
lon: -3.02849
surface_form: great dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.575411111111
lon: -3.0194111111111
The caldera was at least across, and as the caldera collapsed, much more than of magma were erupted. At the close of this volcanic activity, the caldera was filled with sedimentary deposits, represented today by the Seathwaite Fell Sandstone Formation, a sequence of bedded volcaniclastic sandstone and siltstone strata.

Geographic entities mentioned:
surface_form: seathwaite fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.478
lon: -3.192
However, deposition was not confined to the old caldera, and to the east of Thirlmere this formation rests directly on the Birker Fell andesites. On the west ridge of Stybarrow Dodd, the geological map shows a thin deposit of the Seathwaite Fell Sandstone around the 700 m contour. Another caldera volcano then formed in a new area.

Geographic entities mentioned:
surface_form: seathwaite fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.478
lon: -3.192
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
surface_form: stybarrow dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.56105
lon: -3.0175111111111
On the west ridge of Stybarrow Dodd, the geological map shows a thin deposit of the Seathwaite Fell Sandstone around the 700 m contour. Another caldera volcano then formed in a new area. In the area to the north of Sticks Pass, the Birker Fell andesites (and the small area of Seathwaite Fell Sandstone) are overlain by the Lincomb Tarns Tuff Formation.

Geographic entities mentioned:
surface_form: seathwaite fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.478
lon: -3.192
Further to the north-east are an occasional pool and the fallen remains of a wall
Wainwright saw a ‘very loose estate-boundary iron post’, which is no longer present. It may well have been another like the ones found on Sheffield Pike. The only exposed rock is Deepdale Crag, just east of the fallen wall, though this is ‘hardly more than a short stony slope’.

Geographic entities mentioned:
surface_form: sheffield pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.555080555556
lon: -2.9787
From the west there is access to the fell from Stanah on the bridleway to Sticks Pass. From the east, ascents can be made from Glenridding, via Greenside Road and the Sticks Pass bridleway, or via the Sheffield Pike and Green Side ridge. From the north-east ascents can begin from Dockray or High Row, either along the Hart Side ridge or through the rather wet valley of Deepdale.

Geographic entities mentioned:
surface_form: sheffield pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.555080555556
lon: -2.9787
Stybarrow Dodd. Stybarrow Dodd (&quot;the hill of the steep path&quot;) is a mountain or fell in the English Lake District. It stands immediately north of Sticks Pass on the main ridge of the Helvellyn range in the Eastern Fells, which is situated between the lakes of Thirlmere and the Ullswater.

Geographic entities mentioned:
surface_form: helvellyn
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.527230555556
lon: -3.0160527777778
All three are covered by the same sheet of volcanic rock. Topography. The summit of Stybarrow Dodd stands on the main ridge of the Helvellyn range, immediately north of Sticks Pass. This ridge runs north–south for about without dropping below. Stybarrow Dodd occupies just over of this length, from Sticks Pass to the col which connects it to Watson's Dodd and Great Dodd.

Geographic entities mentioned:
surface_form: helvellyn
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.527230555556
lon: -3.0160527777778
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
surface_form: stybarrow dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.56105
lon: -3.0175111111111
Sticks Pass. Sticks Pass, to the south of Stybarrow Dodd, crosses the Helvellyn ridge at a height of about, the highest pass in the Lake District crossed by a bridleway. Now used only by fellwalkers, it once provided a regular connection between the communities on either side of the Helvellyn range. The becks flowing to either side of the pass are both named Sticks Gill on Ordnance Survey maps.

Geographic entities mentioned:
surface_form: helvellyn
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.527230555556
lon: -3.0160527777778
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
surface_form: stybarrow dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.56105
lon: -3.0175111111111
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
Sticks Pass. Sticks Pass, to the south of Stybarrow Dodd, crosses the Helvellyn ridge at a height of about, the highest pass in the Lake District crossed by a bridleway. Now used only by fellwalkers, it once provided a regular connection between the communities on either side of the Helvellyn range. The becks flowing to either side of the pass are both named Sticks Gill on Ordnance Survey maps.

Geographic entities mentioned:
surface_form: helvellyn
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.527230555556
lon: -3.0160527777778
From the east, ascents can be made from Glenridding, via Greenside Road and the Sticks Pass bridleway, or via the Sheffield Pike and Green Side ridge. From the north-east ascents can begin from Dockray or High Row, either along the Hart Side ridge or through the rather wet valley of Deepdale. The summit of Stybarrow Dodd may also be reached from the path along the Helvellyn ridge.

Geographic entities mentioned:
surface_form: helvellyn
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.527230555556
lon: -3.0160527777778
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
surface_form: stybarrow dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.56105
lon: -3.0175111111111
This formation must represent a series of eruptions of truly exceptional magnitude, accompanying the formation of a volcanic caldera, probably in the area around what is now Helvellyn.

Geographic entities mentioned:
surface_form: helvellyn
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.527230555556
lon: -3.0160527777778
Geology. The rocks of Stybarrow Dodd are all part of the Borrowdale Volcanic Group (BVG), formed on the margin of an ancient continent during a period of intense volcanic activity, roughly 450 million years ago in the Ordovician Period. Within that group, the bulk of the rocks forming the fell and its ridges belong to the Birker Fell Andesite Formation.

Geographic entities mentioned:
surface_form: borrowdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.42
lon: -2.665
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
surface_form: stybarrow dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.56105
lon: -3.0175111111111
Stybarrow Dodd. Stybarrow Dodd (&quot;the hill of the steep path&quot;) is a mountain or fell in the English Lake District. It stands immediately north of Sticks Pass on the main ridge of the Helvellyn range in the Eastern Fells, which is situated between the lakes of Thirlmere and the Ullswater.

Geographic entities mentioned:
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
surface_form: stybarrow dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.56105
lon: -3.0175111111111
This ridge is drained by two gills just mentioned, which are now captured by a water leat and diverted into Thirlmere Reservoir. The eastern side of Stybarrow Dodd is more complex and sprawling. Its eastern ridge divides into three parts, with the result that the foot of the mountain stretches along Ullswater from Glenridding to Aira Beck, with two intervening valleys.

Geographic entities mentioned:
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
surface_form: stybarrow dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.56105
lon: -3.0175111111111
The becks flowing to either side of the pass are both named Sticks Gill on Ordnance Survey maps. Alfred Wainwright first added the terms East and West to distinguish them
The route to the pass starts from Stanah in the west and rises over the west ridge of Stybarrow Dodd. It remains to the north of both Sticks Gills, so that most of its length is carried by Stybarrow Dodd.

Geographic entities mentioned:
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
surface_form: stybarrow dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.56105
lon: -3.0175111111111
Alfred Wainwright first added the terms East and West to distinguish them
The route to the pass starts from Stanah in the west and rises over the west ridge of Stybarrow Dodd. It remains to the north of both Sticks Gills, so that most of its length is carried by Stybarrow Dodd. In 1928 the route was still marked by a number of sticks, from which it was supposed that the pass had been named.

Geographic entities mentioned:
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
surface_form: stybarrow dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.56105
lon: -3.0175111111111
The summit of Stybarrow Dodd may also be reached from the path along the Helvellyn ridge. A popular walk known as ‘The Dodds’ combines the three summits of Stybarrow Dodd, Watson's Dodd and Great Dodd, often involving a circuit of Deepdale from High Row or Dockray. Geology.

Geographic entities mentioned:
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
surface_form: stybarrow dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.56105
lon: -3.0175111111111
surface_form: watson's dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5672
lon: -3.02849
surface_form: deepdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.264
lon: -2.432
surface_form: great dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.575411111111
lon: -3.0194111111111
surface_form: deepdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.54
lon: -1.99
Individual lava flows may be separated by beds of volcaniclastic sandstone, sedimentary deposits formed from the erosion of the volcanic rocks. The geological map shows basaltic andesite near Fisher Place, low on the west ridge of Stybarrow Dodd, as well as small amounts of volcaniclastic deposits on the same ridge.

Geographic entities mentioned:
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
surface_form: stybarrow dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.56105
lon: -3.0175111111111
On Stybarrow Dodd this formation is represented by rocks of the Thirlmere Tuff Member, which covers the top of the fell with a thick sheet of welded rhyo-dacitic lapilli tuff in which the individual pieces of semi-molten lava were flattened under the weight of deposits above them.

Geographic entities mentioned:
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
This rock weathers to a white or pink colour, but it is covered by the smooth grassy turf characteristic of Great Dodd, Watson's Dodd and Stybarrow Dodd, all of which are covered by the same sheet. Names. Stybarrow Dodd.

Geographic entities mentioned:
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
surface_form: stybarrow dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.56105
lon: -3.0175111111111
surface_form: stybarrow dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.56105
lon: -3.0175111111111
surface_form: watson's dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5672
lon: -3.02849
surface_form: great dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.575411111111
lon: -3.0194111111111
Names. Stybarrow Dodd. Dodd seems to have been a later addition to the fell's name, which was recorded as &quot;Stibarro&quot; (1589), &quot;Stybrow&quot; (1794) and &quot;Stybarrow&quot; (as late as 1800), although &quot;Stiveray Dod&quot; is also found from about 1692.

Geographic entities mentioned:
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
Probably 'hill of the steep-path,’ named after the path over Sticks Pass on its flanks, from the dialect word &quot;sty(e)&quot; ‘a steep path’ and &quot;berg&quot; (which often becomes &quot;barrow&quot; in place-names) from either the Old English &quot;berg&quot;, ‘a hill’ or Old Norse &quot;berg&quot; ‘a mountain.’
Dod or dodd is a dialect word of unknown origin, but common in hill names in the Lake District and the Scottish Borders for bare rounded summits, either free standing or subsidiary shoulders to higher neighbours.

Geographic entities mentioned:
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
surface_form: barrow
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5858
lon: -3.19703
Within that group, the bulk of the rocks forming the fell and its ridges belong to the Birker Fell Andesite Formation. These rocks are among the earliest of the volcanic rocks of the BVG, and are part of a thick succession of andesite sheets which now outcrop in a wide band around the western and northern sides of the Lake District.

Geographic entities mentioned:
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
This formation is one of the most widespread of the volcanic rocks of the Lake District; it seems that the whole district was buried beneath at least of densely welded ignimbrite, a rock formed from a pyroclastic flow of very hot gas and rock.

Geographic entities mentioned:
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
Its eastern ridge divides into three parts, with the result that the foot of the mountain stretches along Ullswater from Glenridding to Aira Beck, with two intervening valleys. This side is drained by Aira Beck in Deepdale on the north, by Sticks Gill (East) and Glenridding Beck on the south, and by Glencoyne Beck and Mossdale Beck in the two valleys between the ridges.

Geographic entities mentioned:
surface_form: deepdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.264
lon: -2.432
surface_form: deepdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.54
lon: -1.99
There are also two short spurs to the north of the main summit. To the north-west one spur leads down to the col which connects the fell to Watson's Dodd and Great Dodd. To the north-east a longer spur called Middle Tongue runs down into Deepdale, between Browndale Beck and Aira Beck. Sticks Pass.

Geographic entities mentioned:
surface_form: deepdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.264
lon: -2.432
surface_form: deepdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.54
lon: -1.99
It may well have been another like the ones found on Sheffield Pike. The only exposed rock is Deepdale Crag, just east of the fallen wall, though this is ‘hardly more than a short stony slope’. The south-western summit is only lower, but lies on the ridge path, and is marked by a small cairn.

Geographic entities mentioned:
surface_form: deepdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.264
lon: -2.432
surface_form: deepdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.54
lon: -1.99
From the east, ascents can be made from Glenridding, via Greenside Road and the Sticks Pass bridleway, or via the Sheffield Pike and Green Side ridge. From the north-east ascents can begin from Dockray or High Row, either along the Hart Side ridge or through the rather wet valley of Deepdale. The summit of Stybarrow Dodd may also be reached from the path along the Helvellyn ridge.

Geographic entities mentioned:
surface_form: deepdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.264
lon: -2.432
surface_form: hart side
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5693
lon: -2.99297
surface_form: deepdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.54
lon: -1.99
After the eruptions of the Birker Fell Formation the composition of the erupting magma changed from andesitic to dacitic, and as a result the nature of the volcanism became more explosive. A large caldera volcano was built in the area where Scafell and the Langdale Pikes stand today. The caldera was at least across, and as the caldera collapsed, much more than of magma were erupted.

Geographic entities mentioned:
surface_form: scafell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.448
lon: -3.225
This because they rebelled and went on transgressing.&quot;
Two verses later we read: &quot;And ˹remember˺ when We took a covenant from you and raised the mountain above you ˹saying˺, “Hold firmly to that ˹Scripture˺ which We have given you and observe its teachings so perhaps you will become mindful ˹of Allah˺.” Yet you turned away afterwards.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Egypt
coordinates: lat: 28.5384
lon: 33.9752
The national park was set up in September 1995. It is a unique ecosystem with a number of lakes and a large area of pine forests. Spanning an area of about, the national park includes 30 lakes. The three largest lakes are Dryvyaty (fifth largest in the country), Snudy (ninth largest in the country) and Strusta (sixteenth largest in the country). Location.

Geographic entities mentioned:
surface_form: Dryvyaty
instance_of: Lake
countries: Belarus
coordinates: lat: 55.616280555556
lon: 27.028055555556
Second Battle of Sacket's Harbor. The Second Battle of Sacket's Harbor, or simply the Battle of Sacket's Harbor, took place on 29 May 1813, during the War of 1812. A British force was transported across Lake Ontario and attempted to capture the town, which was the principal dockyard and base for the American naval squadron on the lake. Twelve warships were built here.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
The population of Rushon district is 25,800 (1 January 2020 estimate). The district is home to Sarez Lake, which was formed as a result of an earthquake in 1911 in Bartang valley in the east of the district.

Geographic entities mentioned:
surface_form: Sarez Lake
instance_of: Lake
countries: Tajikistan
coordinates: lat: 38.25
lon: 72.616666666667
Machmell River. l8gtb8vk9upaea16ssf97isvqc4i" xml:space="preserve">The Machmell River, also spelled Machmel River, is a river in the Pacific Ranges of the southern Coast Mountains in British Columbia, Canada. It flows west into Owikeno Lake.

Geographic entities mentioned:
surface_form: Owikeno Lake
instance_of: Lake
countries: Canada
coordinates: lat: 51.683333333333
lon: -126.91666666667
The Watauga River downstream of the western side of Elizabethton has one of the only two sections of trophy trout streams in Tennessee. Holston Mountain communication towers. Elizabethton lies within a river valley basin mostly surrounded by mountain ridges and significant hills, such as Holston Mountain, the southern end of which lies just to the northeast.

Geographic entities mentioned:
surface_form: Holston Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.433333333333
lon: -82.133333333333
Mõnnaste. Mõnnaste is a village in Viljandi Parish, Viljandi County, Estonia. Until the 2017 administrative reform of Estonian municipalities the village was located in Tarvastu Parish. Mõnnaste is 15 km (9 miles) southeast of the town of Viljandi near the western shore of the lake Võrtsjärv. The population of Mõnnaste was 69 people as of 2011.

Geographic entities mentioned:
surface_form: Võrtsjärv
instance_of: Lake
countries: Estonia
coordinates: lat: 58.266666666667
lon: 26.033333333333
Ben Hope (disambiguation). d8q9jrnwmj72setgz8lq6mv1u6uo" xml:space="preserve">Ben Hope is a mountain in northern Scotland.

Geographic entities mentioned:
surface_form: Ben Hope
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 58.41355
lon: -4.6087388888889
Poljana, Tuzla. Poljana is a village in the municipality of Tuzla, Tuzla Canton, Bosnia and Herzegovina. It is located at the northeastern tip of Modrac Lake. Demographics. According to the 2013 census, its population was 585.

Geographic entities mentioned:
surface_form: Modrac Lake
instance_of: Lake
countries: Bosnia and Herzegovina
coordinates: lat: 44.49611111
lon: 18.52138889
Life. Paul Mataranga was a feudal lord who held the prestigious title of Sevastocrator. He governed the province of Ghora (also spelled Gora), a region near Lake Ohrid. Although details about his parents, spouse, and early life remain obscure, his position as a ruler highlights his prominence in the region's medieval history.

Geographic entities mentioned:
surface_form: Lake Ohrid
instance_of: Lake
countries: North Macedonia
Albania
coordinates: lat: 41.03333333333333
lon: 20.716666666666665