Sarmila/GeoWiki-Features huggingface dataset:
Etymology. Mount Bernacci, locally known as &quot;Tangcong Vaca&quot;, which translates to “cow’s hump,” is named for its resemblance to the hump of a Brahman cattle. The mountain and the nearby Libmanan caves are collectively referred to as &quot;Hantik&quot; in the local folklore. The origin of its current name, however, remains unknown. Geography and watersheds.

Geographic entities mentioned:
surface_form: tangcong vaca
instance_of: Mountain
countries: Philippines
coordinates: lat: 13.609166666667
lon: 122.97027777778
surface_form: mount bernacci
instance_of: Mountain
countries: Philippines
coordinates: lat: 13.609166666667
lon: 122.97027777778
Mount Bernacci. Mount Bernacci (locally known as Tangcong Vaca) is a mountain in Camarines Sur, Philippines, characterized by its mesa-like profile. It rises to above sea level. The mountain served as the base of operations for the during the Japanese occupation, taking name from the massif.

Geographic entities mentioned:
surface_form: mount bernacci
instance_of: Mountain
countries: Philippines
coordinates: lat: 13.609166666667
lon: 122.97027777778
Incidents. On March 8, 1965, a Filipinas Orient Airways Douglas DC-3A crashed and burned in the slope of Mount Bernacci, as it was approaching Naga Airport. The total fatalities were 10, including 3 crew members. On December 15, 1993, a Philippine Air Force C-130H Hercules crashed on Mount Bernacci. The plane left Manila at 2:17 pm to deliver relief supplies to an area devastated by Typhoon Lola.

Geographic entities mentioned:
surface_form: mount bernacci
instance_of: Mountain
countries: Philippines
coordinates: lat: 13.609166666667
lon: 122.97027777778
They met on the set of &quot;Saturday Night Live&quot; and Juvonen was producer on the film &quot;Fever Pitch&quot;. In August 2007, Fallon proposed on the dock at sunset with a bespoke engagement ring at Nancy's family home in Wolfeboro on Lake Winnipesaukee in New Hampshire. They were married four months later. They have two daughters born in 2013 and 2014.

Geographic entities mentioned:
surface_form: Lake Winnipesaukee
instance_of: Lake
countries: United States
coordinates: lat: 43.598888888889
lon: -71.323055555556
The nephilim can prolong the lives of humans and serve as muses who help to inspire great works of creativity, but they are extremely jealous and will destroy anyone they see as a rival. Crawford and the two poets make their way up the Jungfrau, where it is said one might be able to break the bond with a nephilim.

Geographic entities mentioned:
surface_form: Jungfrau
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.536944444444
lon: 7.9625
Pine Point Formation. The Pine Point Formation is a stratigraphic unit of Givetian age in the Western Canadian Sedimentary Basin. It takes the name from Pine Point, a promontory (and former townsite) on the south shore of the Great Slave Lake, west of Fort Resolution, and was first described in outcrop on the shore of the lake between Pine Point and Fort Resolution by A.E. Cameron in 1918.

Geographic entities mentioned:
surface_form: Great Slave Lake
instance_of: Lake
countries: Canada
coordinates: lat: 61.666666666667
lon: -114
The summit, reaching a height of, lies within Sussex County, New Jersey. Geography. The Hamburg Mountains and Wawayanda Mountain on the east, and Pochuck Mountain to the west, form the borders of the Vernon Valley, an important farming and mining area of New Jersey drained by Pochuck Creek. Geology.

Geographic entities mentioned:
surface_form: Wawayanda Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.1975
lon: -74.4619
surface_form: Pochuck Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.2111
lon: -74.5306
Skeidsberget Hill. Skeidsberget Hill is a hill about 2 nautical miles (3.7 km) northwest of the summit of Skeidshovden Mountain in the Wohlthat Mountains of Queen Maud Land. First photographed from the air by the German Antarctic Expedition (1938–39). Mapped by Norwegian cartographers from surveys and air photos by the Norwegian Antarctic Expedition (1956–60) and named Skeidsberget.

Geographic entities mentioned:
surface_form: Skeidshovden Mountain
instance_of: Mountain
coordinates: lat: -72.13333333
lon: 11.51666667
Mount Nif's mass is a protrusion in western direction of Bozdağlar mountain chain, which separates the valleys of the rivers Gediz and Küçük Menderes, two principal flows of the region, and of which the Mount Bozdağ (Mount Tmolus in antiquity), with its elevation exceeding, constitutes the highest peak, as well as being the highest point for the same region of the provinces of İzmir-Aydın-Manisa-Uşak as a whole.

Geographic entities mentioned:
surface_form: Bozdağlar
instance_of: Mountain
countries: Turkey
coordinates: lat: 38.35525
lon: 27.73949
surface_form: Mount Tmolus
instance_of: Mountain
countries: Turkey
coordinates: lat: 38.35525
lon: 27.73949
surface_form: bozdağlar
instance_of: Mountain
countries: Turkey
coordinates: lat: 38.35525
lon: 27.73949
surface_form: mount tmolus
instance_of: Mountain
countries: Turkey
coordinates: lat: 38.35525
lon: 27.73949
surface_form: tmolus
instance_of: Mountain
countries: Turkey
coordinates: lat: 38.35525
lon: 27.73949
surface_form: mount nif
instance_of: Mountain
countries: Turkey
coordinates: lat: 38.387872
lon: 27.356461
The monument is called &quot;Eti Baba&quot; (&quot;the Hittite father&quot;) locally. A second pass to the north of Mount Nif separates it, or connects it, since it is still at some altitude, from Mount Sipylus, at the locality called &quot;Belkahve&quot;. Belkahve is the principal point of access from the east to İzmir metropolitan area and commands an impressive view of a large part of the city.

Geographic entities mentioned:
surface_form: Mount Sipylus
instance_of: Mountain
countries: Turkey
coordinates: lat: 38.56698
lon: 27.45484
surface_form: sipylus
instance_of: Mountain
countries: Turkey
coordinates: lat: 38.56698
lon: 27.45484
surface_form: mount sipylus
instance_of: Mountain
countries: Turkey
coordinates: lat: 38.56698
lon: 27.45484
surface_form: mount nif
instance_of: Mountain
countries: Turkey
coordinates: lat: 38.387872
lon: 27.356461
Mount Nif. Mount Nif, (elevation:) is a mountain in the district of Kemalpaşa, towering over the district center (formerly also called Nif), located immediately to the east of the city of İzmir, in western Turkey. It was one of the nineteen mountains which carried the name Olympus in ancient times.

Geographic entities mentioned:
surface_form: mount nif
instance_of: Mountain
countries: Turkey
coordinates: lat: 38.387872
lon: 27.356461
Mount Nif is distinguished from the rest of the mountain chain massif by a narrow but key pass at a locality called &quot;Karabel&quot; which leads south towards the town of Torbalı.

Geographic entities mentioned:
surface_form: mount nif
instance_of: Mountain
countries: Turkey
coordinates: lat: 38.387872
lon: 27.356461
Belkahve is the principal point of access from the east to İzmir metropolitan area and commands an impressive view of a large part of the city. Ankara-İzmir highway, notably, is checked by its sinuous slopes. Mount Nif is sometimes cited as &quot;Kemalpaşa Mountain&quot; in reference to the district center, especially in Turkish sources.

Geographic entities mentioned:
surface_form: mount nif
instance_of: Mountain
countries: Turkey
coordinates: lat: 38.387872
lon: 27.356461
Glacial erosion has superficially scoured an elongated area of the Baltic spanning from northern Småland, via Stockholm and Åland to the coast at the Finnish-Russian border. The scoured area and other zones made up of crystalline Fennoscandian Shield rocks (northern and western Baltic Sea) have experienced overall very limited glacial erosion during the Quaternary.

Geographic entities mentioned:
surface_form: Fennoscandian Shield
instance_of: Landform
countries: Norway
Sweden
Finland
Russia
Russian Empire
Soviet Union
coordinates: lat: 63
lon: 17
In its center is a crater lake, Lacus Albanus (Lago Albano), oval in shape, a few km long and wide. At the top of the second-highest peak (Monte Cavo) was a temple to Jupiter Latiaris, where the Latini held state functions before their subjection to Rome, and the Romans subsequently held religious and state ceremonies.

Geographic entities mentioned:
surface_form: Monte Cavo
instance_of: Mountain
countries: Italy
coordinates: lat: 41.751666666667
lon: 12.71
Here, along the narrow plateau above Palazzuola between the Alban lake (&quot;Lagiod di Castello&quot;) and the Alban mount (&quot;Monte Cavo&quot;), extended the town of Alba Longa, which was regarded as the primitive seat of the Latin stock, and the mother city of Rome as well as of all the other Old Latin communities; here on the slopes lay the very ancient Latin districts of Lanuvium, Aricia, and Tusculum.

Geographic entities mentioned:
surface_form: Alban mount
instance_of: Mountain
countries: Italy
coordinates: lat: 41.751666666667
lon: 12.71
Kościelec (High Tatras). Kościelec (2,155 m above sea level) is a mountain in the High Tatras in the Gąsienicowa Valley of Poland. In popular culture. On February 8, 1909, the composer Mieczysław Karłowicz was killed at the age of 32 by an avalanche while skiing in the Little Kościelec. This incident was commemorated by Wojciech Kilar in his tone poem &quot;Kościelec 1909&quot;, composed in 1976.

Geographic entities mentioned:
surface_form: kościelec (high tatras)
instance_of: Mountain
countries: Poland
coordinates: lat: 49.22527778
lon: 20.01444444
Kościelec (High Tatras). Kościelec (2,155 m above sea level) is a mountain in the High Tatras in the Gąsienicowa Valley of Poland. In popular culture. On February 8, 1909, the composer Mieczysław Karłowicz was killed at the age of 32 by an avalanche while skiing in the Little Kościelec. This incident was commemorated by Wojciech Kilar in his tone poem &quot;Kościelec 1909&quot;, composed in 1976.

Geographic entities mentioned:
surface_form: kościelec
instance_of: Mountain
countries: Poland
coordinates: lat: 49.22527778
lon: 20.01444444
Mount Arthur (Nunavut). Mount Arthur is a mountain located on Ellesmere Island, Nunavut, Canada in the Quttinirpaaq National Park. First mapped by the Lady Franklin Bay Expedition, it was named for Chester A. Arthur the 21st President of the United States.

Geographic entities mentioned:
surface_form: island
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
surface_form: mount arthur
instance_of: Mountain
countries: Canada
coordinates: lat: 81.3333
lon: -74.75
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: mount arthur
instance_of: Mountain
countries: Canada
coordinates: lat: 50.1286
lon: -123.917
Mount Arthur (Nunavut). Mount Arthur is a mountain located on Ellesmere Island, Nunavut, Canada in the Quttinirpaaq National Park. First mapped by the Lady Franklin Bay Expedition, it was named for Chester A. Arthur the 21st President of the United States.

Geographic entities mentioned:
surface_form: mount arthur (nunavut)
instance_of: Mountain
countries: Canada
coordinates: lat: 81.3333
lon: -74.75
surface_form: mount arthur
instance_of: Mountain
countries: Canada
coordinates: lat: 50.1286
lon: -123.917
Topography. The topography of the Royal Slope AVA is characterized by the gentle, south-facing slopes of an east–west trending range of hills called the Frenchman Hills. Slope angles are generally less than 15 percent, with very few slopes having angles of less than 3 percent.

Geographic entities mentioned:
surface_form: Frenchman Hills
instance_of: Landform
countries: United States
coordinates: lat: 47
lon: -120
It is the eleventh-highest English Marilyn, standing high, and has a relative height of. It is the highest in the range of fells extending north-west from Great Gable towards Loweswater, and together with its satellites, Red Pike and High Crag, forms a trio of fells overlooking the lake and village of Buttermere. On this side are high crags, wild combes and a small tarn, Bleaberry Tarn.

Geographic entities mentioned:
surface_form: Great Gable
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.482
lon: -3.219
surface_form: Loweswater
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.5825
lon: -3.355277777777778
surface_form: High Crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.514638888889
lon: -3.2681388888889
surface_form: Buttermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.533333333333
lon: -3.2666666666667
surface_form: red pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.483
lon: -3.29
surface_form: high crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.514
lon: -3.0158
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
surface_form: red pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.526
lon: -3.3
It is the highest in the range of fells extending north-west from Great Gable towards Loweswater, and together with its satellites, Red Pike and High Crag, forms a trio of fells overlooking the lake and village of Buttermere. On this side are high crags, wild combes and a small tarn, Bleaberry Tarn. High Stile is most easily ascended as part of a traverse of the three fells. Topography.

Geographic entities mentioned:
surface_form: Bleaberry Tarn
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.527222222222
lon: -3.2902777777778
On this side are high crags, wild combes and a small tarn, Bleaberry Tarn. High Stile is most easily ascended as part of a traverse of the three fells. Topography. The Western Fells occupy a triangular sector of the Lake District, bordered by the River Cocker to the north east and Wasdale to the south east. Westwards the hills diminish toward the coastal plain of Cumberland.

Geographic entities mentioned:
surface_form: Wasdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.425
lon: -3.35
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
Westwards the hills diminish toward the coastal plain of Cumberland. At the central hub of the high country are Great Gable and its satellites, while two principal ridges fan out on either flank of Ennerdale, the western fells in effect being a great horseshoe around this long wild valley.

Geographic entities mentioned:
surface_form: Great Gable
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.482
lon: -3.219
surface_form: ennerdale
instance_of: Valley
countries: United Kingdom
At the central hub of the high country are Great Gable and its satellites, while two principal ridges fan out on either flank of Ennerdale, the western fells in effect being a great horseshoe around this long wild valley. The highest section of the northern branch is formed by the trio of Buttermere fells, High Crag, High Stile and Red Pike.

Geographic entities mentioned:
surface_form: Buttermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.533333333333
lon: -3.2666666666667
surface_form: High Crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.514638888889
lon: -3.2681388888889
surface_form: red pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.483
lon: -3.29
surface_form: high crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.514
lon: -3.0158
surface_form: high stile
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.521669444444
lon: -3.2838111111111
surface_form: red pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.526
lon: -3.3
The highest section of the northern branch is formed by the trio of Buttermere fells, High Crag, High Stile and Red Pike. The Buttermere Fells, also known as Buttermere Edge, form the watershed between Buttermere and Upper Ennerdale. The Ennerdale flanks are steep and rough with areas of crag, the lower slopes being planted with a ribbon of conifers.

Geographic entities mentioned:
surface_form: Buttermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.533333333333
lon: -3.2666666666667
surface_form: buttermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.533333333333
lon: -3.2666666666667
surface_form: buttermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.533333333333
lon: -3.2666666666667
surface_form: ennerdale
instance_of: Valley
countries: United Kingdom
Across the narrow ridge-top to the north are deep corries and dark walls of crag, glowering down over the lake. The ridge continues south east to Haystacks and the Great Gable group. Beyond Red Pike to the west are Starling Dodd, Great Borne and the Loweswater Fells. All three Buttermere Fells throw out a short spur towards the lake with deep combs hollowed out between them.

Geographic entities mentioned:
surface_form: Starling Dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.530180555556
lon: -3.32735
surface_form: Great Borne
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.53435
lon: -3.35685
surface_form: red pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.483
lon: -3.29
surface_form: loweswater
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.5825
lon: -3.355277777777778
surface_form: dodd
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.635
lon: -3.17
surface_form: red pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.526
lon: -3.3
The view is extensive, the highlight perhaps being the North Western Fells across the Buttermere valley. Ennerdale Water and Crummock Water are in view and careful steps toward the brink can also add Bleaberry Tarn to the picture. Fine views of the crags of the surrounding combs complete the foreground. Ascents.

Geographic entities mentioned:
surface_form: Crummock Water
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.55
lon: -3.3
surface_form: bleaberry tarn
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.527222222222
lon: -3.2902777777778
surface_form: ennerdale
instance_of: Valley
countries: United Kingdom
North west of High Stile is Bleaberry Comb, backed by the wall of Chapel Crags. Nestled deep within is Bleaberry Tarn, a pool which is on continual shadow from November to March. Despite the steep contours of the rock walls above, the tarn is only about deep, and is well stocked with trout. Bleaberry Tarn is drained into Buttermere by Sourmilk Gill, reaching the lake mere yards from its outlet.

Geographic entities mentioned:
surface_form: bleaberry tarn
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.527222222222
lon: -3.2902777777778
Nestled deep within is Bleaberry Tarn, a pool which is on continual shadow from November to March. Despite the steep contours of the rock walls above, the tarn is only about deep, and is well stocked with trout. Bleaberry Tarn is drained into Buttermere by Sourmilk Gill, reaching the lake mere yards from its outlet. A belt of trees has been planted along the shoreline.

Geographic entities mentioned:
surface_form: bleaberry tarn
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.527222222222
lon: -3.2902777777778
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
surface_form: buttermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.533333333333
lon: -3.2666666666667
Direct ascents can be made if desired via either of the northern combs. From the shore of Buttermere a path runs up into Birkness Comb from where the northern spur can be gained. From Buttermere village the path to Bleaberry Tarn can be used, branching off to find a line around the eastern end of Chapel Crags. If climbing from Ennerdale the route up Red Pike may be used.

Geographic entities mentioned:
surface_form: bleaberry tarn
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.527222222222
lon: -3.2902777777778
A belt of trees has been planted along the shoreline. Birkness Comb, also called Burtness Comb on Ordnance Survey maps, lies between the truncated and unnamed northern ridges of High Crag and High Stile. The lack of a retaining moraine means that this hollow has no tarn, Comb Beck running uninterrupted to the Lake. Grey Crag and Eagle Crag are the main faces on High Stile.

Geographic entities mentioned:
surface_form: high crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.514638888889
lon: -3.2681388888889
surface_form: high crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.514
lon: -3.0158
surface_form: high stile
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.521669444444
lon: -3.2838111111111
The northern slopes display the underlying olistostrome of disrupted, sheared and folded mudstone, siltstone and sandstone of the Buttermere Formation. In the direction of Red Pike are intrusions of the granophyric granite. In Burtness Comb, a prominent bank of debris runs along the outer flank of the upper cirque, then turns down into the lower cirque, ending in a block strew at the intake wall.

Geographic entities mentioned:
surface_form: red pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.483
lon: -3.29
surface_form: red pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.526
lon: -3.3
Direct ascents can be made if desired via either of the northern combs. From the shore of Buttermere a path runs up into Birkness Comb from where the northern spur can be gained. From Buttermere village the path to Bleaberry Tarn can be used, branching off to find a line around the eastern end of Chapel Crags. If climbing from Ennerdale the route up Red Pike may be used.

Geographic entities mentioned:
surface_form: red pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.483
lon: -3.29
surface_form: red pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.526
lon: -3.3
surface_form: ennerdale
instance_of: Valley
countries: United Kingdom
The lack of a retaining moraine means that this hollow has no tarn, Comb Beck running uninterrupted to the Lake. Grey Crag and Eagle Crag are the main faces on High Stile. These corries being scooped out of the northern face result in the connecting ridges between the three Buttermere Fells being fine and narrow.

Geographic entities mentioned:
surface_form: eagle crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.499
lon: -3.12097
surface_form: grey crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.457680555556
lon: -2.7773888888889
surface_form: high stile
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.521669444444
lon: -3.2838111111111
There are no paths on the southern flank of High Stile. Geology. The summit area is formed of the siltstone, sandstone, conglomerate, tuff, lapilli tuff and andesite sills of the Eagle Crag Member. The northern slopes display the underlying olistostrome of disrupted, sheared and folded mudstone, siltstone and sandstone of the Buttermere Formation.

Geographic entities mentioned:
surface_form: eagle crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.499
lon: -3.12097
In Burtness Comb, a prominent bank of debris runs along the outer flank of the upper cirque, then turns down into the lower cirque, ending in a block strew at the intake wall. It marks the course of a rock avalanche which fell from Grey Crag on the summit rim of High Stile, and was channeled along the foot of the glacier some 11,000 years ago. It is unique in the Lake District.

Geographic entities mentioned:
surface_form: grey crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.457680555556
lon: -2.7773888888889
surface_form: high stile
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.521669444444
lon: -3.2838111111111
This was worked from 1569 to 1570 and again in the 1820s. Summit. The highest point lies a little way out onto the northern spur at the top of Grey Crag, marked by a cairn. The highest point on the main ridge is only lower and was regarded as the summit by Alfred Wainwright, the maps available at the time not deciding the issue. This top has two main cairns side by side.

Geographic entities mentioned:
surface_form: grey crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.457680555556
lon: -2.7773888888889
This top has two main cairns side by side. In an attempt to avoid confusion some guidebooks refer to the summit as Grey Crag and the top on the ridge as High Stile. The view is extensive, the highlight perhaps being the North Western Fells across the Buttermere valley. Ennerdale Water and Crummock Water are in view and careful steps toward the brink can also add Bleaberry Tarn to the picture.

Geographic entities mentioned:
surface_form: grey crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.457680555556
lon: -2.7773888888889
surface_form: high stile
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.521669444444
lon: -3.2838111111111
Ascents. The fell is usually ascended as a traverse of the ‘Buttermere Three’, as the north eastern flank is very steep and rough. Strong walkers may continue the walk towards Haystacks, southeast. The direct ascent from Ennerdale (through forest and steep bracken) is not found in guidebooks. The fell is climbed as part of &quot;Variation 1&quot; on the Coast to Coast Walk.

Geographic entities mentioned:
surface_form: haystacks
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.508
lon: -3.248
These corries being scooped out of the northern face result in the connecting ridges between the three Buttermere Fells being fine and narrow. The Ennerdale flanks have a tier of crag at around, The Knors and Raven Crag being the principal features. At the foot of the slopes are the massed conifers of the Ennerdale Forest, all contributing to the difficulty of access.

Geographic entities mentioned:
surface_form: raven crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5596
lon: -3.07778
surface_form: ennerdale
instance_of: Valley
countries: United Kingdom
High Stile. High Stile is a mountain in the western part of the Lake District in North West England. It is the eleventh-highest English Marilyn, standing high, and has a relative height of.

Geographic entities mentioned:
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
surface_form: high stile
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.521669444444
lon: -3.2838111111111
The ridge continues south east to Haystacks and the Great Gable group. Beyond Red Pike to the west are Starling Dodd, Great Borne and the Loweswater Fells. All three Buttermere Fells throw out a short spur towards the lake with deep combs hollowed out between them. North west of High Stile is Bleaberry Comb, backed by the wall of Chapel Crags.

Geographic entities mentioned:
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
surface_form: buttermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.533333333333
lon: -3.2666666666667
A belt of trees has been planted along the shoreline. Birkness Comb, also called Burtness Comb on Ordnance Survey maps, lies between the truncated and unnamed northern ridges of High Crag and High Stile. The lack of a retaining moraine means that this hollow has no tarn, Comb Beck running uninterrupted to the Lake. Grey Crag and Eagle Crag are the main faces on High Stile.

Geographic entities mentioned:
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
It marks the course of a rock avalanche which fell from Grey Crag on the summit rim of High Stile, and was channeled along the foot of the glacier some 11,000 years ago. It is unique in the Lake District. There are the remains of a small copper-mine near the shore of Buttermere. This was worked from 1569 to 1570 and again in the 1820s. Summit.

Geographic entities mentioned:
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
Grey Crag and Eagle Crag are the main faces on High Stile. These corries being scooped out of the northern face result in the connecting ridges between the three Buttermere Fells being fine and narrow. The Ennerdale flanks have a tier of crag at around, The Knors and Raven Crag being the principal features.

Geographic entities mentioned:
surface_form: buttermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.533333333333
lon: -3.2666666666667
Geology. The summit area is formed of the siltstone, sandstone, conglomerate, tuff, lapilli tuff and andesite sills of the Eagle Crag Member. The northern slopes display the underlying olistostrome of disrupted, sheared and folded mudstone, siltstone and sandstone of the Buttermere Formation. In the direction of Red Pike are intrusions of the granophyric granite.

Geographic entities mentioned:
surface_form: buttermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.533333333333
lon: -3.2666666666667
It marks the course of a rock avalanche which fell from Grey Crag on the summit rim of High Stile, and was channeled along the foot of the glacier some 11,000 years ago. It is unique in the Lake District. There are the remains of a small copper-mine near the shore of Buttermere. This was worked from 1569 to 1570 and again in the 1820s. Summit.

Geographic entities mentioned:
surface_form: buttermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.533333333333
lon: -3.2666666666667
This top has two main cairns side by side. In an attempt to avoid confusion some guidebooks refer to the summit as Grey Crag and the top on the ridge as High Stile. The view is extensive, the highlight perhaps being the North Western Fells across the Buttermere valley. Ennerdale Water and Crummock Water are in view and careful steps toward the brink can also add Bleaberry Tarn to the picture.

Geographic entities mentioned:
surface_form: buttermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.533333333333
lon: -3.2666666666667
Fine views of the crags of the surrounding combs complete the foreground. Ascents. The fell is usually ascended as a traverse of the ‘Buttermere Three’, as the north eastern flank is very steep and rough. Strong walkers may continue the walk towards Haystacks, southeast. The direct ascent from Ennerdale (through forest and steep bracken) is not found in guidebooks.

Geographic entities mentioned:
surface_form: buttermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.533333333333
lon: -3.2666666666667
The fell is climbed as part of &quot;Variation 1&quot; on the Coast to Coast Walk. Direct ascents can be made if desired via either of the northern combs. From the shore of Buttermere a path runs up into Birkness Comb from where the northern spur can be gained. From Buttermere village the path to Bleaberry Tarn can be used, branching off to find a line around the eastern end of Chapel Crags.

Geographic entities mentioned:
surface_form: buttermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.533333333333
lon: -3.2666666666667
surface_form: buttermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.533333333333
lon: -3.2666666666667
High Stile. High Stile is a mountain in the western part of the Lake District in North West England. It is the eleventh-highest English Marilyn, standing high, and has a relative height of.

Geographic entities mentioned:
surface_form: high stile
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.521669444444
lon: -3.2838111111111
It is the highest in the range of fells extending north-west from Great Gable towards Loweswater, and together with its satellites, Red Pike and High Crag, forms a trio of fells overlooking the lake and village of Buttermere. On this side are high crags, wild combes and a small tarn, Bleaberry Tarn. High Stile is most easily ascended as part of a traverse of the three fells. Topography.

Geographic entities mentioned:
surface_form: high stile
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.521669444444
lon: -3.2838111111111
Beyond Red Pike to the west are Starling Dodd, Great Borne and the Loweswater Fells. All three Buttermere Fells throw out a short spur towards the lake with deep combs hollowed out between them. North west of High Stile is Bleaberry Comb, backed by the wall of Chapel Crags. Nestled deep within is Bleaberry Tarn, a pool which is on continual shadow from November to March.

Geographic entities mentioned:
surface_form: high stile
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.521669444444
lon: -3.2838111111111
The Ennerdale flanks have a tier of crag at around, The Knors and Raven Crag being the principal features. At the foot of the slopes are the massed conifers of the Ennerdale Forest, all contributing to the difficulty of access. There are no paths on the southern flank of High Stile. Geology.

Geographic entities mentioned:
surface_form: high stile
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.521669444444
lon: -3.2838111111111
The Buttermere Fells, also known as Buttermere Edge, form the watershed between Buttermere and Upper Ennerdale. The Ennerdale flanks are steep and rough with areas of crag, the lower slopes being planted with a ribbon of conifers. Across the narrow ridge-top to the north are deep corries and dark walls of crag, glowering down over the lake.

Geographic entities mentioned:
surface_form: ennerdale
instance_of: Valley
countries: United Kingdom
The Ennerdale flanks have a tier of crag at around, The Knors and Raven Crag being the principal features. At the foot of the slopes are the massed conifers of the Ennerdale Forest, all contributing to the difficulty of access. There are no paths on the southern flank of High Stile. Geology.

Geographic entities mentioned:
surface_form: ennerdale
instance_of: Valley
countries: United Kingdom
Ascents. The fell is usually ascended as a traverse of the ‘Buttermere Three’, as the north eastern flank is very steep and rough. Strong walkers may continue the walk towards Haystacks, southeast. The direct ascent from Ennerdale (through forest and steep bracken) is not found in guidebooks. The fell is climbed as part of &quot;Variation 1&quot; on the Coast to Coast Walk.

Geographic entities mentioned:
surface_form: ennerdale
instance_of: Valley
countries: United Kingdom
The two troops withdrew with the 1st Armoured Brigade when it retreated on 8 April and reached Perdikkas by the following day. The regiment and E Troop, 5th Field Regiment, were the only units left on the plain between Mount Olympus and the Aliakmon on 8 April. The next day, A Squadron demolished the main bridge across the Aliakmon, after the 1st Armoured Brigade had withdrawn southward.

Geographic entities mentioned:
surface_form: Mount Olympus
instance_of: Mountain
countries: Greece
coordinates: lat: 40.083333333333336
lon: 22.35
The next day, A and C Squadrons withdrew from Olympus Pass and Eleftherochorion after a German tank attack. B Squadron fought a rearguard action at Tempe, retreating down the Volos road and losing several carriers. The regiment, reunited on the Volos road, retreated to the Thermopylae Line. On 21 April it was ordered to patrol Euboea but its vehicles were too badly damaged to do so.

Geographic entities mentioned:
surface_form: Tempe
instance_of: Valley
countries: Greece
coordinates: lat: 39.872778
lon: 22.546667
On 6 January, the regiment left Bardia for Baggush, returning to Maadi on 26 January. Syria and Rommel's second offensive. On 13 March, the New Zealand Division moved to Syria to build fortifications in the Beqaa Valley, to protect against the prospect of an Axis attack from Turkey. The regiment had to build roads at Laboue and Wadi Fa'rah, camping at Djedeida.

Geographic entities mentioned:
surface_form: Beqaa Valley
instance_of: Valley
countries: Lebanon
coordinates: lat: 34.008888888889
lon: 36.145277777778
Lake Belle Taine is a lake in Hubbard County, Minnesota, United States. The lake was first named by the settlers of Hubbard County as &quot;Elbow Lake&quot; for its sharply bent outlines. Its name in Ojibwe is &quot;Gaa-aachaajigwaatigweyaag zaaga'igan&quot; meaning &quot;the lake into which the river pitches and ceases to flow,—dies there&quot; due to it having no visible outlet.

Geographic entities mentioned:
surface_form: elbow lake
instance_of: Lake
countries: United States
coordinates: lat: 46.8343363
lon: -122.4568674
surface_form: elbow lake
instance_of: Lake
countries: United States
coordinates: lat: 46.00833333
lon: -96.00833333
Lake Belle Taine. Lake Belle Taine is a lake in Hubbard County, Minnesota, United States. The lake was first named by the settlers of Hubbard County as &quot;Elbow Lake&quot; for its sharply bent outlines.

Geographic entities mentioned:
surface_form: lake belle taine
instance_of: Lake
countries: United States
coordinates: lat: 46.94335
lon: -94.88697
Marden, Wiltshire. Marden is a small village and civil parish southeast of Devizes in the county of Wiltshire, south west England. The parish is in the Vale of Pewsey which carries the upper section of the Salisbury Avon; to the south the parish extends into Salisbury Plain. History. A settlement of 29 households and one mill was recorded at &quot;Meresdene&quot; in Domesday Book of 1086.

Geographic entities mentioned:
surface_form: Vale of Pewsey
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.352
lon: -1.851
The site is set in the Warta River floodplain and is surrounded by marshes. It is an important wintering location for migratory waterbirds such as geese and ducks. The site is a diverse wetland system around Wigry Lake and 42 smaller glacial lakes surrounded by boreal woodlands. The location shelters three globally endangered bird species, red kite (), white-tailed eagle () and corn crake ().

Geographic entities mentioned:
surface_form: Wigry Lake
instance_of: Lake
countries: Poland
coordinates: lat: 54.036666666667
lon: 23.098333333333
Honors. In a ceremony before their July 9, 2005, game against the St. Louis Cardinals, the Giants honored Nen with a plaque commemorating his 300th career save. The plaque is now located on the public walkway behind the right-field wall of Oracle Park, not far from McCovey Cove.

Geographic entities mentioned:
surface_form: McCovey Cove
instance_of: Body of water
countries: United States
coordinates: lat: 37.7772
lon: -122.388
Flora Haines Loughead. Flora Haines Loughead (later, Flora Gutierrez; 1855–1943) was an American writer, farmer, and miner from Wisconsin. She became the &quot;Opal Queen&quot; of Virgin Valley. Flora's son Allan was the founder of American aerospace company the Lockheed Corporation. Early years and education.

Geographic entities mentioned:
surface_form: Virgin Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.8025
lon: -114.082
Mining. Her next career started in 1915 when she was sent to investigate the discovery of opals in Virgin Valley, Nevada, from San Francisco. She was reporting for the &quot;San Francisco Chronicle&quot; but she decided to buy 15 claims years after homesteading on Sagebrugh Creek at the Green Fire Mine (Sinkakis- Gemstones of North America).

Geographic entities mentioned:
surface_form: Virgin Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.8025
lon: -114.082
The counterintuitive direction of water flow is because the Continental Divide forms a loop in this area, whereby the peak's west slope runoff flows to the Atlantic Ocean and the east slope to the Pacific. Topographic relief is significant as the summit rises above the Kawuneeche Valley in and over above the South Fork Michigan River in. Etymology.

Geographic entities mentioned:
surface_form: Kawuneeche Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.3563
lon: -105.859
The islands are rugged and rocky with some low peaks; the coasts are mostly cliffs. The highest point is Slættaratindur in northern Eysturoy, above sea level. The Faroe Islands are made up of an approximately six-kilometres-thick succession of mostly basaltic lava that was part of the great North Atlantic Igneous Province during the Paleogene period.

Geographic entities mentioned:
surface_form: Slættaratindur
instance_of: Mountain
countries: Faroe Islands
coordinates: lat: 62.2967169
lon: -7.0132
Singleton Nunatak. mm5ejguqk229xrr57sifeqozsvj" xml:space="preserve">#redirect Singleton Nunatak

Geographic entities mentioned:
surface_form: singleton nunatak
instance_of: Mountain
coordinates: lat: -71.25
lon: -61.6
Ricardo Palma Bridge. Ricardo Palma Bridge () is a reinforced concrete beam bridge that crosses the Rímac river, connecting Abancay Avenue with Jirón Hualgayoc and thus connecting the districts of Lima and Rímac, both part of the historic centre of Lima, the capital city of Peru. It is named after the Peruvian author, scholar, librarian and politician Ricardo Palma.

Geographic entities mentioned:
surface_form: Rímac river
instance_of: Watercourse
countries: Peru
coordinates: lat: -12.032222222222
lon: -77.141111111111
Erythronium quinaultense. &quot;Erythronium quinaultense&quot;, the Quinault fawn-lily, is a rare plant species endemic to a small region around Lake Quinault in Olympic National Park, Washington state, United States. &quot;Erythronium quinaultense&quot; produces egg-shaped bulbs up to long. Leaves are up to long. Scape is up to long, bearing one to three flowers.

Geographic entities mentioned:
surface_form: Lake Quinault
instance_of: Lake
countries: United States
coordinates: lat: 47.476377777778
lon: -123.87016388889
George Peak. George Peak, at, is the second highest peak in the Raft River Mountains of Utah. The peak is located in Sawtooth National Forest and Box Elder County. It is west of Bull Mountain and can be accessed via forest road 009, which travels near the summit. Climate. George Creek is a SNOTEL weather station situated on the northern face of George Peak, at an elevation of 9005 feet (2745 m).

Geographic entities mentioned:
surface_form: bull mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.9117
lon: -113.365
surface_form: bull
instance_of: Watercourse
countries: United States
coordinates: lat: 49.46663
lon: -115.45205
surface_form: bull mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.140277777778
lon: -110.73222222222
George Peak. George Peak, at, is the second highest peak in the Raft River Mountains of Utah. The peak is located in Sawtooth National Forest and Box Elder County. It is west of Bull Mountain and can be accessed via forest road 009, which travels near the summit. Climate. George Creek is a SNOTEL weather station situated on the northern face of George Peak, at an elevation of 9005 feet (2745 m).

Geographic entities mentioned:
surface_form: george peak
instance_of: Mountain
countries: United States
coordinates: lat: 41.8891
lon: -113.483
It is west of Bull Mountain and can be accessed via forest road 009, which travels near the summit. Climate. George Creek is a SNOTEL weather station situated on the northern face of George Peak, at an elevation of 9005 feet (2745 m). George Creek has a subalpine climate (Köppen &quot;Dfc&quot;), bordering on a humid continental climate (Köppen &quot;Dfb&quot;).

Geographic entities mentioned:
surface_form: george peak
instance_of: Mountain
countries: United States
coordinates: lat: 41.8891
lon: -113.483
The Sel Church is located about north of the town centre, just outside the town proper. Geography. Situated about north of Lillehammer, it spans the valley floor where the Ottadalen valley branches off of the main Gudbrandsdalen valley. The largely glacially-fed river Otta has a watershed in a very arid region and all of this water flows into the river Gudbrandsdalslågen at the town of Otta.

Geographic entities mentioned:
surface_form: Ottadalen
instance_of: Valley
countries: Norway
coordinates: lat: 61.833333333333
lon: 9.2333333333333
surface_form: Gudbrandsdalen
instance_of: Valley
countries: Norway
coordinates: lat: 61.1333
lon: 10.35
Transportation. Otta sits roughly halfway between the major cities of Oslo and Trondheim along the European route E6 highway. The Norwegian National Road starts at Otta and it heads west through the Ottadalen valley and over the mountains to Stryn Municipality, along the Nordfjord, finally terminating in the town of Måløy on the west coast of Norway.

Geographic entities mentioned:
surface_form: Ottadalen
instance_of: Valley
countries: Norway
coordinates: lat: 61.833333333333
lon: 9.2333333333333
Over time, a small village grew up around the railway station. In 1912, the railroad was completed from Otta to Dombås in 1912, and then ultimately being completed all the way to Trondheim in 1922. On 28 April 1940, Otta saw extensive fighting between German and British forces during the last parts of the German advance up the Gudbrandsdalen valley, as part of the German conquest of Norway.

Geographic entities mentioned:
surface_form: Gudbrandsdalen
instance_of: Valley
countries: Norway
coordinates: lat: 61.1333
lon: 10.35
This list is organized by major coastline. States with large numbers of beaches are listed on linked subarticles. District of Columbia. The District of Columbia does not currently have a true beach; several areas (such as Georgetown Waterfront Park) have boundaries along the Potomac River, but lack a true beach. From 1914 to 1925, there was a beach at the District of Columbia’s Tidal Basin.

Geographic entities mentioned:
surface_form: Tidal Basin
instance_of: Lake
countries: United States
coordinates: lat: 38.884166666666665
lon: -77.03916666666667
The British managed to escape, but Walter Butler was killed. Background. New York's Mohawk Valley had been a major area of internecine warfare throughout the American Revolution. By 1780 raids conducted by British soldiers, mercenaries, loyalist militia, and their Mohawk allies had devastated the valley.

Geographic entities mentioned:
surface_form: Mohawk Valley
instance_of: Valley
countries: United States
The lichen is found in wet grasslands and upland peat bogs. Taxonomy. &quot;Protopannaria campbellensis&quot; was first described as a new species by Dag Øvstedal and Alan Fryday in 2011. The type specimen was discovered on the summit of Mount Dumas on Campbell Island, New Zealand, at an altitude of. The species name, &quot;campbellensis&quot;, refers to its discovery location. Description.

Geographic entities mentioned:
surface_form: Mount Dumas
instance_of: Mountain
countries: New Zealand
coordinates: lat: -52.571133
lon: 169.098458
The region is fertile, with ample precipitation and an abundance of flora and fauna, lessening the need to travel far for food. Historical, physical items (such as the weirs and fish traps found in Lake Condah, south of Hamilton), as well as Aboriginal accounts of early white settlers, support the local oral histories of well-established, pre-European settlements in the area. British colonisation.

Geographic entities mentioned:
surface_form: Lake Condah
instance_of: Lake
countries: Australia
coordinates: lat: -38.093159
lon: 141.794924
Competition for food with the introduced rabbits is another major issue affecting the marsupials. Within the city, the public lands adjoining the river and Lake Hamilton have been subject to spasmodic tree-planting projects. Mount Napier—the highest point on the Western District Plains—is found south of Hamilton. Education.

Geographic entities mentioned:
surface_form: Mount Napier
instance_of: Mountain
countries: Australia
coordinates: lat: -37.894
lon: 142.059
Route. The northern end of the Byway begins at the intersection of SH 82 and SH 133 in Carbondale. The route follows SH 133 south down the Crystal River Valley past Mount Sopris and Redstone to McClure Pass, with an official detour option to Marble. The true Loop portion of the Byway begins and ends below Paonia Reservoir and The Raggeds where Kebler Pass intersects SH 133.

Geographic entities mentioned:
surface_form: Mount Sopris
instance_of: Mountain
countries: United States
coordinates: lat: 39.2632
lon: -107.176