Sarmila/GeoWiki-Features huggingface dataset:
In 1887, the Lehigh Valley Railroad obtained a lease on the Southern Central Railroad (the LVRR previously had trackage rights on the railroad starting in 1870), which had a route from Sayre northward into the Finger Lakes region. At the same time, the LVRR organized the Buffalo and Geneva Railroad to build the rest of the 97-mile Geneva to Buffalo trackage, from Geneva to Lancaster.

Geographic entities mentioned:
surface_form: Finger Lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 42.666666666667
lon: -76.833333333333
Also, in 1914 the Panama Canal was completed, and the LVRR gained an important new market with ores shipped from South America to the Bethlehem Steel company. In order to handle the additional new ocean traffic, the LVRR created a large new pier at Constable Hook, which opened in 1915, and a new terminal at Claremont which opened in 1923. It also built a passenger terminal in Buffalo in 1915.

Geographic entities mentioned:
surface_form: Constable Hook
instance_of: Landform
countries: United States
coordinates: lat: 40.6578
lon: -74.0994
It also built a passenger terminal in Buffalo in 1915. Since 1896 the LVRR had run an important and prestigious express train named the &quot;Black Diamond&quot; which carried passengers to the Finger Lakes and Buffalo. Additional passenger trains ran from Philadelphia to Scranton and westward.

Geographic entities mentioned:
surface_form: Finger Lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 42.666666666667
lon: -76.833333333333
This primarily consisted of the main line and related branches from Van Etten Junction (north of Sayre, Pennsylvania) to Oak Island Yard, the Ithaca branch from Van Etten Junction to Ithaca, New York, connecting to the Cayuga Lake line and on to the Milliken power station in Lake Ridge, New York (closed on August 29, 2019) and the Cargill salt mine just south of Auburn, and small segments in Geneva, New York(from Geneva to the Seneca Army Depot in Kendaia), Batavia, New York, Auburn, New York, and Cortland, New York.

Geographic entities mentioned:
surface_form: Cayuga Lake
instance_of: Lake
countries: United States
coordinates: lat: 42.68805555555556
lon: -76.70222222222222
To the northeast stretch the Großes Moor (near Vechta) and the hill of the Kellenberg; east of the ridge is the Dümmer, and behind it the Stemweder Berg, to the south – on the other side of the Großes Moor (near Damme) – are the Wiehen Hills in the North Teutoburg Forest-Wiehen Hills Nature Park and to the west on the other side of the Hase valley are the Ankum Heights. Watersheds.

Geographic entities mentioned:
surface_form: Dümmer
instance_of: Lake
countries: Germany
coordinates: lat: 52.5
lon: 8.35
The Lingen Heights, the Ankum Heights, the Kellenberg and the Brelinger Berg also belong to this push moraine, also called the &quot;Rehburg Phase&quot;, which can be dated to about 230,000 years ago. The Rehburg Hills by the lake of the Steinhuder Meer, are not, however, part of the moraine.

Geographic entities mentioned:
surface_form: Steinhuder Meer
instance_of: Lake
countries: Germany
coordinates: lat: 52.466666666667
lon: 9.3333333333333
It is part of the &quot;comarca&quot; of Horta Sud. Paiporta was billed as the ground zero of the October 2024 floods affecting the province of Valencia. In the town, 45 inhabitants died. In the case of Paiporta and other municipalities of the Valencia metropolitan area, damage was caused by the overflow of the Rambla del Poyo.

Geographic entities mentioned:
surface_form: Rambla del Poyo
instance_of: Watercourse
countries: Spain
coordinates: lat: 39.378611111111
lon: -0.35638888888889
The surrounding peaks are generally accessible to hikers and climbers only by traversing the length of the glacier itself. From the Vrenelisgärtli peak, the Lake Klontal may be seen directly, more than one mile below. In recent years, the glacier has lost a massive amount of its volume and its tongue has retreated sharply. East of the Glärnisch is located the lower Vorder Glärnisch.

Geographic entities mentioned:
surface_form: Vorder Glärnisch
instance_of: Mountain
countries: Switzerland
coordinates: lat: 47.0225
lon: 9.04151
It consists of several summits, of which the highest, &quot;Bächistock&quot;, is 2,915 metres above sea level. Until 2013, the highest point was considered to be an unnamed point with a summit cross at 2,914 metres (until 2013: 2'915 metres). The other main summits are &quot;Vrenelisgärtli&quot; (&quot;Verena's Little Garden&quot; at 2,904 metres) and the &quot;Ruchen&quot; (2,901 metres).

Geographic entities mentioned:
surface_form: ruchen
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.956472222222
lon: 9.2446666666667
The other main summits are &quot;Vrenelisgärtli&quot; (&quot;Verena's Little Garden&quot; at 2,904 metres) and the &quot;Ruchen&quot; (2,901 metres). The massif of the Glärnisch consists of two ridges of either side of the glacier named &quot;Glärnischfirn&quot;, culminating at the Ruchen to the west, rising more than 2,000 metres above the Klöntalersee, and at the Bächistock to the southwest.

Geographic entities mentioned:
surface_form: ruchen
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.956472222222
lon: 9.2446666666667
Glärnisch. The Glärnisch is a mountain massif of the Schwyz Alps, overlooking the valley of the Linth in the Swiss canton of Glarus. It consists of several summits, of which the highest, &quot;Bächistock&quot;, is 2,915 metres above sea level. Until 2013, the highest point was considered to be an unnamed point with a summit cross at 2,914 metres (until 2013: 2'915 metres).

Geographic entities mentioned:
surface_form: glärnisch
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.998611111111
lon: 8.9986111111111
The Vrenelisgärtli is the closest peak to Schwanden. The Glärnischfirn (also known as the Glärnischgletscher, the &quot;Glarnisch Glacier&quot;) is about one mile long and about one-half mile wide at between 1.5 and 2.0 miles above sea level. The surrounding peaks are generally accessible to hikers and climbers only by traversing the length of the glacier itself.

Geographic entities mentioned:
surface_form: glarnisch
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.998611111111
lon: 8.9986111111111
On June 14, 1877, as the various groups of Nez Perces gathered near Tolo Lake before finally rejoining the reservation, several young Nez Perces belonging to White Bird's group set out along the Salmon River to avenge the death of a relative killed by whites a few years earlier. Back at camp, they announced that they had killed four men and wounded another.

Geographic entities mentioned:
surface_form: Tolo Lake
instance_of: Lake
countries: United States
coordinates: lat: 45.915561111111
lon: -116.2361
Windy Valley. cb54ructd7t85br2vsgx6iq0d4fi" xml:space="preserve">#redirect Windy Valley

Geographic entities mentioned:
surface_form: windy valley
instance_of: Valley
coordinates: lat: -68.6167
lon: -66.8333
It then passes Kiana, entering its broad delta approximately 10 miles (16 km) southwest of town. The Kobuk empties into the Hotham Inlet of Kotzebue Sound approximately 30 miles (48 km) southeast of the city of Kotzebue. History. The Kobuk's Inuit name, &quot;Kuuvak&quot;, means &quot;great river&quot;. It was first transcribed by John Simpson in 1850 as &quot;Kowuk&quot;.

Geographic entities mentioned:
surface_form: Hotham Inlet
instance_of: Landform
countries: United States
coordinates: lat: 66.819722222222
lon: -161.965
For example, it rises above the Bering Glacier to the south in about. Mount Steller is the high point of Waxell Ridge, an east–west trending ridge on the south side of the Bagley Icefield, one of the largest icefields in North America. The large Bering Glacier flows past the east and south slopes of the ridge, while the Steller Glacier flows from its west side.

Geographic entities mentioned:
surface_form: high point
instance_of: Mountain
countries: United States
coordinates: lat: 41.924722222222
lon: -74.288055555556
surface_form: mount steller
instance_of: Mountain
countries: United States
coordinates: lat: 60.5203
lon: -143.091
surface_form: high point
instance_of: Mountain
countries: United States
coordinates: lat: 41.3209
lon: -74.6616
surface_form: mount steller
instance_of: Mountain
countries: United States
coordinates: lat: 58.4297
lon: -154.391
Mount Steller (Chugach Mountains). Mount Steller is a peak at the far eastern end of the Chugach Mountains of Alaska, United States. It is notable for its isolated location among extensive icefields, and for its large rise above local terrain. For example, it rises above the Bering Glacier to the south in about.

Geographic entities mentioned:
surface_form: mount steller
instance_of: Mountain
countries: United States
coordinates: lat: 60.5203
lon: -143.091
surface_form: mount steller
instance_of: Mountain
countries: United States
coordinates: lat: 58.4297
lon: -154.391
The large Bering Glacier flows past the east and south slopes of the ridge, while the Steller Glacier flows from its west side. The mountain was named for the naturalist Georg Wilhelm Steller. Due to its isolated location, poor weather, and comparatively low absolute elevation by Alaskan standards, Mount Steller was not climbed until recently. The first ascent was in 1992. Climate.

Geographic entities mentioned:
surface_form: mount steller
instance_of: Mountain
countries: United States
coordinates: lat: 60.5203
lon: -143.091
surface_form: mount steller
instance_of: Mountain
countries: United States
coordinates: lat: 58.4297
lon: -154.391
The first ascent was in 1992. Climate. Based on the Köppen climate classification, Mount Steller is located in a subarctic climate zone with long, cold, snowy winters, and mild summers. Weather systems coming off the Gulf of Alaska are forced upwards by the Chugach Mountains (orographic lift), causing heavy precipitation in the form of rainfall and snowfall.

Geographic entities mentioned:
surface_form: mount steller
instance_of: Mountain
countries: United States
coordinates: lat: 60.5203
lon: -143.091
surface_form: mount steller
instance_of: Mountain
countries: United States
coordinates: lat: 58.4297
lon: -154.391
Bràigh nan Uamhachan. Braigh nan Uamhachan (765 m) is a mountain in the Northwest Highlands of Scotland. It is located north of Glenfinnan in Lochaber. Taking the form of a long ridge, the climb is steep and pathless, but provides fantastic views of all the neighbouring peaks from its summit.

Geographic entities mentioned:
surface_form: braigh nan uamhachan
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.926284
lon: -5.3291575
Bràigh nan Uamhachan. Braigh nan Uamhachan (765 m) is a mountain in the Northwest Highlands of Scotland. It is located north of Glenfinnan in Lochaber. Taking the form of a long ridge, the climb is steep and pathless, but provides fantastic views of all the neighbouring peaks from its summit.

Geographic entities mentioned:
surface_form: bràigh nan uamhachan
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.926284
lon: -5.3291575
Lake of Orient. The Lake of Orient or Seine Reservoir Lake is a lake in northeastern France, located in the Aube department of the Grand Est region. With a surface area of and a normal capacity of, it is the third-largest Artificial Lake in mainland France, after Lake Der-Chantecoq and Lake Serre-Ponçon, and ahead of Lake Sainte-Croix.

Geographic entities mentioned:
surface_form: lake of orient
instance_of: Lake
countries: France
coordinates: lat: 48.2725
lon: 4.33
Geography. The Lake of Orient is located in the Champagne wetlands, 12 km east of Troyes in the Aube department (Champagne-Ardenne), in the heart of the Oriental forest. This forest, which gave the lake its name, was named after the Knights Templar, who owned part of the site in the Middle Ages.

Geographic entities mentioned:
surface_form: lake of orient
instance_of: Lake
countries: France
coordinates: lat: 48.2725
lon: 4.33
Today, however, even the Regional Natural Park uses the name &quot;The Lake of Orient&quot;. On May 7, 2013, the filling level of the Lake of Orient became exceptionally high. The Public Territorial Basin Establishment decided to continue filling the Orient, Temple and Amance lakes up to a limit of 50 cm.

Geographic entities mentioned:
surface_form: lake of orient
instance_of: Lake
countries: France
coordinates: lat: 48.2725
lon: 4.33
Since 2003, the cycling path known as the Lake Cycling Way (&quot;Vélovoie des lacs&quot;) has linked Saint-Julien-les-Villas to the outskirts of Troyes and Dienville, running along the Saint Julien Canal, the Morge Canal, the shores of the Lake of Orient and Temple Lake for a total of 42 km.

Geographic entities mentioned:
surface_form: lake of orient
instance_of: Lake
countries: France
coordinates: lat: 48.2725
lon: 4.33
The company opened a new computer chip factory near Chengdu shortly after Zhou left his post in Sichuan. He also focused on improving tourism resources, significantly revamping the Mount Emei scenic region to attract more visitors. Zhou also improved public safety in the province, for example, by enacting policies that aimed to reduce accidents in the province's water lanes.

Geographic entities mentioned:
surface_form: Mount Emei
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 29.519722222222
lon: 103.3325
Sandungen. Sandungen is the name of two lakes in Nordmarka in Oslo, Norway. Store Sandungen has an area of 2.9 km², and the nearby Vesle Sandungen covers 1.4 km².

Geographic entities mentioned:
surface_form: sandungen
instance_of: Lake
countries: Norway
coordinates: lat: 60.116
lon: 10.621
Sandungen. Sandungen is the name of two lakes in Nordmarka in Oslo, Norway. Store Sandungen has an area of 2.9 km², and the nearby Vesle Sandungen covers 1.4 km².

Geographic entities mentioned:
surface_form: sandungen
instance_of: Lake
countries: Norway
coordinates: lat: 60.116
lon: 10.621
surface_form: sandungen
instance_of: Lake
countries: Norway
coordinates: lat: 60.116
lon: 10.621
Scotts Peak. Scotts Peak is a mountain in South West Tasmania which is associated with the construction and flooding of the original Lake Pedder, as the lake now completely surrounds the peak. It lies east of the Frankland Range and has an elevation of 669 metres. There is a Scotts Peak Dam and a Scotts Peak Dam Road in the region.

Geographic entities mentioned:
surface_form: scotts peak
instance_of: Mountain
countries: Australia
coordinates: lat: -43.004
lon: 146.279
It lies east of the Frankland Range and has an elevation of 669 metres. There is a Scotts Peak Dam and a Scotts Peak Dam Road in the region. Scotts Peak is accessible by Scotts Peak Dam Road and the Lake Pedder boat ramp. Many people kayak across the reservoir to hike Scotts Peak. Climate.

Geographic entities mentioned:
surface_form: scotts peak
instance_of: Mountain
countries: Australia
coordinates: lat: -43.004
lon: 146.279
surface_form: scotts peak
instance_of: Mountain
countries: Australia
coordinates: lat: -43.004
lon: 146.279
There is a Scotts Peak Dam and a Scotts Peak Dam Road in the region. Scotts Peak is accessible by Scotts Peak Dam Road and the Lake Pedder boat ramp. Many people kayak across the reservoir to hike Scotts Peak. Climate. Due to its far south-western location, this site is frequently lashed by severe weather; with a mean annual wind speed of, peaking at a mean of in September.

Geographic entities mentioned:
surface_form: scotts peak
instance_of: Mountain
countries: Australia
coordinates: lat: -43.004
lon: 146.279
De Ménageot also took her to see the Villa Aldobrandini, and the ancient ruins of the Roman town of Tusculum, which &quot;evoked many sad thoughts&quot;. T‌he entourage continued to Monte Cavo, seeking out the Temple of Jupiter built there. She visited numerous villas, including the Villa Conti, the Villa Palavicina and the ruins of Hadrian's Villa.

Geographic entities mentioned:
surface_form: Monte Cavo
instance_of: Mountain
countries: Italy
coordinates: lat: 41.751666666667
lon: 12.71
As she arrived in Naples she was captivated by the view of the city, the distant plumes of smoke from Mount Vesuvius, the rolling hills of the countryside, and its citizens, writing &quot;...even the people, so lively, so boisterous, so different from the people of Rome, that one would think a thousand leagues lay between the two cities&quot;.

Geographic entities mentioned:
surface_form: Mount Vesuvius
instance_of: Mountain
countries: Italy
coordinates: lat: 40.821388888889
lon: 14.425555555556
She continued to Venice, passing Trevi, Cetri and Foligno. In the latter town she found Raphael's &quot;Madonna di Foligno,&quot; which gained the complete admiration of Le Brun. She continued to Perugia, passing by Lake Trasimene and hen on to Lise, Combuccia, Arezzo, Levana and Pietre-Fonte, finally arriving in Florence, where she had resided for a short while after her flight from France.

Geographic entities mentioned:
surface_form: Lake Trasimene
instance_of: Lake
countries: Italy
coordinates: lat: 43.14
lon: 12.1
She visited the Madonna del Monte, enjoying its commanding view, and sketched the countryside frequently. She later visited Lake Maggiore and resided on one of the two islands in the lake, the Isola Bella, being granted permission by the Prince Borromeo to lodge on the estate there. She soon attempted to visit the other isle, Isola Madre, but stormy weather affected her journey and she returned.

Geographic entities mentioned:
surface_form: Lake Maggiore
instance_of: Lake
countries: Switzerland
Italy
coordinates: lat: 46.098055555555554
lon: 8.714722222222223
All I can tell you is that my soul gloried in such a solemn and melancholy vision. She returned to Soleure the next day, and then departed for Vevey, which she described as &quot;the land of my dreams&quot;. She rented a house on the banks of Lake Geneva and toured the countryside and mountains around Vevey. She walked up Mount Blonay where the Messieurs de Blonay hosted her at Blonay castle.

Geographic entities mentioned:
surface_form: Lake Geneva
instance_of: Lake
countries: Switzerland
France
coordinates: lat: 46.45
lon: 6.55
After returning from Coppet to Geneva, where she was made an honorary member of the Société pour l'Avancement des Beaux-Arts, she departed in a group with the de Brac family for Chamonix, intending to visit the Sallanches mountains, the Aiguille du Goûter, and Mont Blanc. The journey was perilous. The entourage visited the Bossons Glacier. On the way upwards, M.

Geographic entities mentioned:
surface_form: Aiguille du Goûter
instance_of: Mountain
countries: France
coordinates: lat: 45.85055556
lon: 6.83111111
surface_form: Mont Blanc
instance_of: Mountain
countries: France
Italy
coordinates: lat: 45.83277777777778
lon: 6.865
Switzerland in 1808. With her desire for travel still not sated, Vigée Le Brun re-entered Switzerland in 1808 via Neuchâtel, and then visited Lucerne, where she was enchanted by the picturesque and wild town. The artist also visited Brown and the market town of Schwyz, then Zug, where she crossed Lake Zug. She visited an inn where she wanted to visit the infamous landslide of Goldau.

Geographic entities mentioned:
surface_form: Lake Zug
instance_of: Lake
countries: Switzerland
coordinates: lat: 47.116666666667
lon: 8.4833333333333
The Pasterze, Austria's most extended glacier, lies on the Grossglockner's eastern slope. The characteristic pyramid-shaped peak actually consists of two pinnacles, the &quot;Großglockner&quot; and the Kleinglockner (, from German: &quot;groß&quot; 'big', &quot;klein&quot; 'small'), separated by the &quot;Glocknerscharte&quot; col. Etymology.

Geographic entities mentioned:
surface_form: Kleinglockner
instance_of: Mountain
countries: Austria
coordinates: lat: 47.073888888889
lon: 12.696111111111
surface_form: kleinglockner
instance_of: Mountain
countries: Austria
coordinates: lat: 47.073888888889
lon: 12.696111111111
surface_form: großglockner
instance_of: Mountain
countries: Austria
coordinates: lat: 47.074528
lon: 12.69385
The region around the mountain has formed part of the Grossglockner-Pasterze special protected area within the High Tauern National Park since 1986. The Glockner is the highest mountain in the Alps east of the Ortler range, about away, and, after Mont Blanc, has the second greatest topographic isolation of all mountains in the Alps.

Geographic entities mentioned:
surface_form: Mont Blanc
instance_of: Mountain
countries: France
Italy
coordinates: lat: 45.83277777777778
lon: 6.865
It ranges out to or, taking account of atmospheric refraction, almost. Its view over more than of the Earth's surface reaches as far as the Upper Swabian Plateau in the northwest, to Regensburg and the peaks of the Bohemian Forest in the north, to Ortler in the west, to the Padan Plain in the south, and to Triglav and the Totes Gebirge range in the east. Topography.

Geographic entities mentioned:
surface_form: Ortler
instance_of: Mountain
countries: Italy
coordinates: lat: 46.508888888889
lon: 10.545
surface_form: Padan Plain
instance_of: Valley
countries: Italy
coordinates: lat: 45.330277777778
lon: 9.7988888888889
surface_form: Triglav
instance_of: Mountain
countries: Slovenia
coordinates: lat: 46.378333
lon: 13.836667
It runs northeastwards and borders on the Northeast and North Faces of the Grossglockner. The latter faces are bounded by the Northwest Ridge, part of the main Glockner crest, which runs over the &quot;Grögerschneid&quot;, and the ridge elevations of Glocknerhorn, and Teufelshorn, to the &quot;Untere Glocknerscharte&quot;, which connects to the high Glocknerwand.

Geographic entities mentioned:
surface_form: Glocknerwand
instance_of: Mountain
countries: Austria
coordinates: lat: 47.079722222222
lon: 12.686388888889
surface_form: glocknerwand
instance_of: Mountain
countries: Austria
coordinates: lat: 47.079722222222
lon: 12.686388888889
A first ascent by skiing was made in 1909 and the circumnavigation of the massif soon became a popular ski mountaineering tour. The Grossglockner became Austria's highest mountain, when the South Tyrolean Ortler region had to be ceded to the Kingdom of Italy according to the 1919 Treaty of Saint-Germain, which promoted its reputation as a tourist attraction. High Alpine Road.

Geographic entities mentioned:
surface_form: Ortler
instance_of: Mountain
countries: Italy
coordinates: lat: 46.508888888889
lon: 10.545
Grossglockner. The Großglockner (), or just Glockner, is, at 3,798 metres above the Adriatic (12,461 ft), the highest mountain in Austria and highest mountain in the Alps east of the Brenner Pass. It is part of the larger Glockner Group of the Hohe Tauern range, situated along the main ridge of the Central Eastern Alps and the Alpine divide.

Geographic entities mentioned:
surface_form: glockner
instance_of: Mountain
countries: Austria
coordinates: lat: 47.074528
lon: 12.69385
surface_form: großglockner
instance_of: Mountain
countries: Austria
coordinates: lat: 47.074528
lon: 12.69385
Grossglockner. The Großglockner (), or just Glockner, is, at 3,798 metres above the Adriatic (12,461 ft), the highest mountain in Austria and highest mountain in the Alps east of the Brenner Pass. It is part of the larger Glockner Group of the Hohe Tauern range, situated along the main ridge of the Central Eastern Alps and the Alpine divide.

Geographic entities mentioned:
surface_form: glockner
instance_of: Mountain
countries: Austria
coordinates: lat: 47.074528
lon: 12.69385
The denotation &quot;Glogger&quot; is mentioned in a 1583 description of the Tyrolean Kals legal district, then referring to the whole ridge south of the Alpine main chain. In the 1760s, the &quot;Atlas Tyrolensis&quot; listed a &quot;Glockner Berg&quot;, the prefix &quot;Gross-&quot; (&quot;great&quot;) is not mentioned before the first expedition in 1799.

Geographic entities mentioned:
surface_form: glockner
instance_of: Mountain
countries: Austria
coordinates: lat: 47.074528
lon: 12.69385
The &quot;Obere Glocknerscharte&quot; between the two peaks, at, is the highest col in Austria, from which a couloir up to 55° in gradient and in altitude descends down to the &quot;Glocknerkees&quot; glacier, called &quot;Pallavicinirinne&quot; after the Austrian mountaineer Alfred von Pallavicini (1848–1886).

Geographic entities mentioned:
surface_form: glockner
instance_of: Mountain
countries: Austria
coordinates: lat: 47.074528
lon: 12.69385
The peak is part of the &quot;Glocknerkamm&quot; ridge in the Glockner Group that branches off the main chain of the Alps at Eiskögele, heading in a southeasterly direction and forming the boundary between the East Tyrolean municipality of Kals am Großglockner, about in the southwest at, and Carinthian Heiligenblut, about in the northeast at.

Geographic entities mentioned:
surface_form: großglockner
instance_of: Mountain
countries: Austria
coordinates: lat: 47.074528
lon: 12.69385
Grossglockner. The Großglockner (), or just Glockner, is, at 3,798 metres above the Adriatic (12,461 ft), the highest mountain in Austria and highest mountain in the Alps east of the Brenner Pass. It is part of the larger Glockner Group of the Hohe Tauern range, situated along the main ridge of the Central Eastern Alps and the Alpine divide.

Geographic entities mentioned:
surface_form: grossglockner
instance_of: Mountain
countries: Austria
coordinates: lat: 47.074528
lon: 12.69385
It is part of the larger Glockner Group of the Hohe Tauern range, situated along the main ridge of the Central Eastern Alps and the Alpine divide. The Pasterze, Austria's most extended glacier, lies on the Grossglockner's eastern slope.

Geographic entities mentioned:
surface_form: grossglockner
instance_of: Mountain
countries: Austria
coordinates: lat: 47.074528
lon: 12.69385
He travelled the Eastern Alps from 1779 to 1781 and published an itinerary in 1783, describing the &quot;Glokner&quot; mountain and stating that it had not been climbed yet. He estimated the mountain's height with converted and left an engraving illustrating Grossglockner and Pasterze, the first known depiction of the mountain. First ascent.

Geographic entities mentioned:
surface_form: grossglockner
instance_of: Mountain
countries: Austria
coordinates: lat: 47.074528
lon: 12.69385
First ascent. Inspired by Hacquet's book and the first ascent of the Mont Blanc in 1786, the Gurk prince-bishop Count Franz Xaver of Salm (1749–1822) together with his vicar general Sigismund Ernst Hohenwart (1745–1825) and Baron Franz Xaver von Wulfen (1728–1805) started efforts for a Grossglockner expedition.

Geographic entities mentioned:
surface_form: grossglockner
instance_of: Mountain
countries: Austria
coordinates: lat: 47.074528
lon: 12.69385
The vanguard reached the Kleinglockner peak, however, according to the expedition records by the Dellach priest Franz Joseph Horasch (Orasch), only the four guides and Mathias Hautzendorfer, the local priest of the Rangersdorf parish, were able to cross the &quot;Obere Glocknerscharte&quot; and climb the Grossglockner summit.

Geographic entities mentioned:
surface_form: grossglockner
instance_of: Mountain
countries: Austria
coordinates: lat: 47.074528
lon: 12.69385
The two &quot;Glockners&quot; are usually identified as the brothers Joseph (&quot;Sepp&quot;) and Martin Klotz, however, this surname is not listed in the Heiligenblut parish register. A local peasant named Sepp Hoysen is documented as a member of the second Grossglockner expedition in 1802, and the surveyor Ulrich Schiegg mentioned one Martin Reicher as &quot;Glockner&quot; guide.

Geographic entities mentioned:
surface_form: grossglockner
instance_of: Mountain
countries: Austria
coordinates: lat: 47.074528
lon: 12.69385
A local peasant named Sepp Hoysen is documented as a member of the second Grossglockner expedition in 1802, and the surveyor Ulrich Schiegg mentioned one Martin Reicher as &quot;Glockner&quot; guide. The peasants and several other members of the expedition (among them Schiegg and his young apprentice Valentin Stanič, who climbed Mt.

Geographic entities mentioned:
surface_form: grossglockner
instance_of: Mountain
countries: Austria
coordinates: lat: 47.074528
lon: 12.69385
Pseudotropheus brevis. &quot;Pseudotropheus brevis&quot; is a species of cichlid endemic to Lake Malawi where it is found in Nkudzi Bay and Monkey Bay in rocky areas. This species can reach a length of SL. It can also be found in the aquarium trade.

Geographic entities mentioned:
surface_form: Lake Malawi
instance_of: Lake
countries: Malawi
Mozambique
Tanzania
coordinates: lat: -12.183333333333
lon: 34.366666666667
Perkins Lake (Oregon). Perkins Lake is a lake on the central Oregon Coast that is located in the Oregon dunes along Highway 101, in Douglas County. It is approximately in size and it is stocked with rainbow trout by the Oregon Department of Fish and Wildlife.

Geographic entities mentioned:
surface_form: perkins lake
instance_of: Lake
countries: United States
coordinates: lat: 43.8262
lon: -124.1494
They exist for other band witnesses written of two megalithic monuments, situated in Montjuïc and Field of the Harp, of those that nevertheless has not remained any rastre material.

Geographic entities mentioned:
surface_form: Montjuïc
instance_of: Mountain
countries: Spain
coordinates: lat: 41.364166666667
lon: 2.1580555555556
Apparently, it had a wall with two accesses, while located outside the walls there was a set of silos with 44 deposits carved into the rock. The main Iberian settlement in the area was in Montjuïc, possibly the 'Barkeno', although the urbanization of the mountain in recent years and its intensive use as a stone quarry throughout the history of the city has caused the loss of most remains.

Geographic entities mentioned:
surface_form: Montjuïc
instance_of: Mountain
countries: Spain
coordinates: lat: 41.364166666667
lon: 2.1580555555556
It is confined mostly to the Mojave Desert between elevation. It thrives in the open grasslands of Queen Valley and Lost Horse Valley in Joshua Tree National Park. Other regions with a large population of the trees can be found northeast of Kingman, Arizona, in Mohave County; and along U.S.

Geographic entities mentioned:
surface_form: Lost Horse Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.001441666667
lon: -116.17778333333
He started selling gum, and transitioned to real estate shortly after. By 1946, he founded the Trousdale Construction Company. He built tract homes and neighborhoods that came with churches and shopping centers, mostly in minority areas located in Long Beach, Wilmington, Compton and the San Fernando Valley. He borrowed money from Bank of America to finance his projects.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
This discovery, like so many others which have been fraught with great import to humanity, was purely an accidental one, and it eventually led to a true appreciation of the value of the mineral on the part of the general public, and to its being mined and placed on the market.|pp73-74 HISTORY OF CARBON COUNTY, Chapter VI<ref
name=claims>Nungesser, pp73-74 HISTORY OF CARBON COUNTY, Chapter VI: spends 3-4 paragraphs discussing Black stone known for centuries to the Indians, was known in the Wyoming Valley, &quot;was early suspected on the headwaters of the Schuylkill&quot;, etc.

Geographic entities mentioned:
surface_form: Wyoming Valley
instance_of: Valley
countries: United States
coordinates: lat: 41.251
lon: -75.906
The parish had a population of 5,794 at the 2011 census. History. Nailsworth in ancient times was a settlement at the confluence of the Avening Valley and the Woodchester Valley, on the Nailsworth Stream. Among many notable historic medieval buildings in the area are Beverston Castle and Owlpen Manor. Nailsworth Town Hall, built as a chapel for a dissenting congregation, was completed in 1867.

Geographic entities mentioned:
surface_form: Avening Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.6811
lon: -2.17472
The first complete genome was submitted to NCBI in 2019. Available genomes place it as a member inside &quot;Xanthomonas arboricola&quot;. Distribution. Unknown in stonefruit in California until detection in Sacramento and northern San Joaquin Valley in the spring of 2013. it is still restricted to those two areas. Also found in almond cultivation in Victoria, Australia. Detection.

Geographic entities mentioned:
surface_form: San Joaquin Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.628888888889
lon: -120.185
Angara-Vitim batholith. uixlttrs1hce6ay87kkcn874prwot" xml:space="preserve">The Angara-Vitim batholith is group of plutons in the eastern Siberia, just east of Lake Baikal. The batholith formed in the Devonian–Early Carboniferous likely in connection to a mantle plume. It formed about the same time and by the same process as the Kalba-Narym batholith in eastern Kazakhstan.

Geographic entities mentioned:
surface_form: Lake Baikal
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.30277778
lon: 108.00472222
According to the 2020 census, it has a population of 99,725 as of 2020. Putatan is located at the south of the City of Manila. It is bounded by barangays Alabang and Bayanan on the north, Laguna de Bay on the east, the Muntinlupa Poblacion on the south; and barangay Ayala Alabang on the west. The barangay is also home to the city hall of Muntinlupa and its several departments. Etymology.

Geographic entities mentioned:
surface_form: Laguna de Bay
instance_of: Lake
countries: Philippines
coordinates: lat: 14.508888888889
lon: 121.11888888889
Lake Peace. Lake Peace was a post ice-age glacial lake in what is now the Peace River basin in northeastern British Columbia and northwestern Alberta.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: lake peace
instance_of: Lake
countries: Canada
Lake Peace. Lake Peace was a post ice-age glacial lake in what is now the Peace River basin in northeastern British Columbia and northwestern Alberta.

Geographic entities mentioned:
surface_form: lake peace
instance_of: Lake
countries: Canada
The bog-free sides of Parlick make it more popular with walkers than the shallow boggy hills to its north. Paths zigzag up this hill from the south, or for the more strenuous ascent a straight path can be chosen. This hill is usually green &mdash; different from the often thorny brown to red of the northern hills. A thin neck joins Parlick onto Fair Snape Fell with well-worn paths linking the two.

Geographic entities mentioned:
surface_form: Fair Snape Fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.919361111111
lon: -2.6150888888889
surface_form: parlick
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.8998
lon: -2.6167
surface_form: fair snape fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.919361111111
lon: -2.6150888888889
A thin neck joins Parlick onto Fair Snape Fell with well-worn paths linking the two. The summit consists of little more than a flat collection of stones, leaving the walker to look at the view, south to Preston and Winter Hill near Chorley, east toward Pendle Hill, and west towards Blackpool and the Irish Sea.

Geographic entities mentioned:
surface_form: Pendle Hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.869
lon: -2.3
surface_form: winter hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.63
lon: -2.515
Parlick. Parlick (also known as Parlick Pike) is an approximately cone-shaped steep-sided hill at the extreme south of the main range of Bowland fells in Lancashire, England. It has an elevation of above sea level. Recreation. Parlick has an elevation of above sea level and a prominence of about.

Geographic entities mentioned:
surface_form: parlick
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.8998
lon: -2.6167
Parlick. Parlick (also known as Parlick Pike) is an approximately cone-shaped steep-sided hill at the extreme south of the main range of Bowland fells in Lancashire, England. It has an elevation of above sea level. Recreation. Parlick has an elevation of above sea level and a prominence of about.

Geographic entities mentioned:
surface_form: parlick
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.8998
lon: -2.6167
surface_form: parlick
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.8998
lon: -2.6167
It has an elevation of above sea level. Recreation. Parlick has an elevation of above sea level and a prominence of about. The bog-free sides of Parlick make it more popular with walkers than the shallow boggy hills to its north. Paths zigzag up this hill from the south, or for the more strenuous ascent a straight path can be chosen.

Geographic entities mentioned:
surface_form: parlick
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.8998
lon: -2.6167
Recreation. Parlick has an elevation of above sea level and a prominence of about. The bog-free sides of Parlick make it more popular with walkers than the shallow boggy hills to its north. Paths zigzag up this hill from the south, or for the more strenuous ascent a straight path can be chosen. This hill is usually green &mdash; different from the often thorny brown to red of the northern hills.

Geographic entities mentioned:
surface_form: parlick
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.8998
lon: -2.6167
The extensive west-facing bowl allows paraglider pilots to fly to Fair Snape Fell and beyond without leaving reliable ridge lift and as far forwards as Beacon Fell. Local pilots use this arena for club competitions, such as the 'Parlick Grid Challenge'
The boundary between the boroughs of Wyre and Ribble Valley passes very close to the summit, with half of the hill lying within each borough.

Geographic entities mentioned:
surface_form: parlick
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.8998
lon: -2.6167
Local aspects. The hill and its environs are the location of the legend of the enormous Dun Cow, which was reputed to wander freely across the moorland, and to be in the habit of quenching its thirst at &quot;Nick's Water-Pot&quot;, a well on the summit of Parlick. &quot;Parlick Fell&quot; is the name of a cheese made in Longridge from sheep's milk from the area.

Geographic entities mentioned:
surface_form: parlick
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.8998
lon: -2.6167
surface_form: parlick
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.8998
lon: -2.6167
Parlick is a popular venue for foot-launched and conventional gliders, because it produces good ridge lift in an unusually wide variety of wind directions. The extensive west-facing bowl allows paraglider pilots to fly to Fair Snape Fell and beyond without leaving reliable ridge lift and as far forwards as Beacon Fell.

Geographic entities mentioned:
surface_form: fair snape fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.919361111111
lon: -2.6150888888889
surface_form: beacon fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.3069
lon: -3.11
Amundsen Glacier. The Amundsen Glacier () is a major Antarctic glacier, about 7 to 11 km (4 to 6 nmi) wide and 150 km (80 nmi) long. It originates on the Antarctic Plateau where it drains the area to the south and west of Nilsen Plateau, then descends through the Queen Maud Mountains to enter the Ross Ice Shelf just west of the MacDonald Nunataks. Name.

Geographic entities mentioned:
surface_form: Antarctic Plateau
instance_of: Plateau
coordinates: lat: -90
lon: 0
surface_form: Nilsen Plateau
instance_of: Plateau
coordinates: lat: -86.3333
lon: -158
surface_form: MacDonald Nunataks
instance_of: Mountain
coordinates: lat: -85.45
lon: -157.633
It flows northwest to the Nødtvedt Nunataks, which it passes on both sides, and is fed by the Norway Glacier from the left (west) south of Mount Hassel, where it wheels to the north and then northeast, fed by Devils Glacier from the left, by the Epler Glacier from the right and then by the Christy Glacier from the left.

Geographic entities mentioned:
surface_form: Nødtvedt Nunataks
instance_of: Mountain
coordinates: lat: -86.5333
lon: -162.3
The tributary Blackwall Glacier flows northwest along the northeast side of Hansen Spur to join Amundsen Glacier. It flows north through past Beck Peak and the Breyer Mesa. Continuing north it is joined by the Tate Glacier, Moffett Glacier and Whitney Glacier from the left, and by the Cappellari Glacier to the right.

Geographic entities mentioned:
surface_form: Beck Peak
instance_of: Mountain
coordinates: lat: -86.0833
lon: -158.967
surface_form: Breyer Mesa
instance_of: Mountain
coordinates: lat: -86.0167
lon: -161.2
It flows north through past Beck Peak and the Breyer Mesa. Continuing north it is joined by the Tate Glacier, Moffett Glacier and Whitney Glacier from the left, and by the Cappellari Glacier to the right. As it enters the Ross Ice Shelf between Witalis Peak and the MacDonald Nunataks it converges with the Bowman Glacier on the left and the Goodale Glacier on the right. Norway Glacier.

Geographic entities mentioned:
surface_form: Witalis Peak
instance_of: Mountain
coordinates: lat: -85.55
lon: -160.3
surface_form: MacDonald Nunataks
instance_of: Mountain
coordinates: lat: -85.45
lon: -157.633
Devils Glacier. A heavily crevassed glacier at the edge of the polar plateau, about long and wide, draining the south part of the Mohn Basin and flowing northeast to enter the upper part of Amundsen Glacier just north of the mountain group consisting of Mount Wisting, Mount Hassel, Mount Bjaaland and Mount Prestrud.

Geographic entities mentioned:
surface_form: Mohn Basin
instance_of: Landform
coordinates: lat: -86.5
lon: -168
Amundsen's route southward, between 168° and 169°W, took the party across the upper or western portion of the glacier. Christy Glacier. A steep tributary glacier draining southeast along the southwest side of Breyer Mesa to enter Amundsen Glacier. Mapped by United States Geological Survey (USGS) from surveys and United States Navy air photos, 1960-64. Named by US-ACAN for Clarence C.

Geographic entities mentioned:
surface_form: Breyer Mesa
instance_of: Mountain
coordinates: lat: -86.0167
lon: -161.2
Mapped by USGS from surveys and USN air photos, 1960-64. Named by US-ACAN for Robert Tate, geomagnetist / seismologist with the South Pole Station winter party, 1964. Moffett Glacier. A tributary glacier, long, flowing east from Rawson Plateau to enter Amundsen Glacier just south of Mount Benjamin. Discovered by R. Admiral Byrd on the South Pole flight of Nov. 28-29, 1929, and named by him for R.

Geographic entities mentioned:
surface_form: Mount Benjamin
instance_of: Mountain
coordinates: lat: -85.8
lon: -160.1
Discovered and mapped by the ByrdAE, 1928-30. Named by US-ACAN for Raymond L. Whitney, meteorologist, South Pole Station winter party, 1961. Bowman Glacier. A deeply entrenched glacier, long, descending the polar plateau between Quarles Range and Rawson Plateau of the Queen Maud Mountains to enter the Ross Ice Shelf just west of the flow of Amundsen Glacier.

Geographic entities mentioned:
surface_form: Rawson Plateau
instance_of: Mountain
coordinates: lat: -85.8667
lon: -164.75
Steagall Glacier. A tributary glacier, long, draining the east slopes of Rawson Plateau between Mount Alice Gade and Mount Deardorff and flowing north to enter Bowman Glacier. First mapped by the Byrd Antarctic Expedition, 1928–30. Named by US-ACAN for Jack Steagall, meteorologist, South Pole Station winter party, 1961. Epler Glacier.

Geographic entities mentioned:
surface_form: Mount Alice Gade
instance_of: Mountain
coordinates: lat: -85.75
lon: -163.667
surface_form: Mount Deardorff
instance_of: Mountain
coordinates: lat: -85.8
lon: -162.567
First mapped by the Byrd Antarctic Expedition, 1928–30. Named by US-ACAN for Jack Steagall, meteorologist, South Pole Station winter party, 1961. Epler Glacier. A tributary glacier, long, draining west from Nilsen Plateau to enter Amundsen Glacier just south of Olsen Crags. Mapped by USGS from surveys and USN air photos, 1960-64. Named by US-ACAN for Charles F.

Geographic entities mentioned:
surface_form: Nilsen Plateau
instance_of: Plateau
coordinates: lat: -86.3333
lon: -158
Mapped by USGS from surveys and USN air photos, 1960-64. Named by US-ACAN for Charles F. Epler, storekeeper with USN Squadron VX-6 on Operation Deep Freeze 1966 and 1967. Blackwall Glacier. A tributary glacier, long, which drains a portion of the west slope of Nilsen Plateau. It flows northwest along the northeast side of Hansen Spur to join Amundsen Glacier.

Geographic entities mentioned:
surface_form: Nilsen Plateau
instance_of: Plateau
coordinates: lat: -86.3333
lon: -158
The name was used by both the 1963-64 and 1970-71 Ohio State University field parties at Nilsen Plateau; all the rock walls surrounding this glacier are black in appearance. Cappellari Glacier. A glacier long in the Hays Mountains, flowing west from the northwest shoulder of Mount Vaughan to enter Amundsen Glacier just north of Mount Dort. First roughly mapped by the ByrdAE, 1928-30.

Geographic entities mentioned:
surface_form: Mount Vaughan
instance_of: Mountain
coordinates: lat: -85.916666666667
lon: -155.83333333333
surface_form: Mount Dort
instance_of: Mountain
coordinates: lat: -85.9
lon: -158.883
Named by US-ACAN for Lewis K. Cappellari who made ionospheric studies at McMurdo Station in 1965. Goodale Glacier. A glacier which flows north from Mount Goodale and Mount Armstrong along the west side of Medina Peaks, in the foothills of the Queen Maud Mountains. First seen and mapped by the ByrdAE, 1928-30. Named by US-ACAN in association with Mount Goodale. Head of glacier.

Geographic entities mentioned:
surface_form: Mount Goodale
instance_of: Mountain
coordinates: lat: -85.75
lon: -157.717
surface_form: Medina Peaks
instance_of: Mountain
coordinates: lat: -85.6
lon: -155.9
Botniahalvøya. Botniahalvøya is a peninsula of Nordaustlandet, Svalbard. It is located between Lady Franklinfjorden and Brennevinsfjorden. It has a length of about twelve nautical miles. The highest peak is Franklinfjellet, at 430 m.a.s.l.

Geographic entities mentioned:
surface_form: Franklinfjellet
instance_of: Mountain
countries: Norway
coordinates: lat: 80.2365
lon: 19.2254
The Gulen fjord branches off the Frøysjøen to the east. The main settlements along the fjord include Kalvåg and Berle on the western shore. The mountain Hornelen lies along the shore of the fjord, northeast of Berle. The fjord connects with the open ocean on the west end and it connects to the Nordfjorden on the northeast end. The fjord is a main shipping lane between the towns of Måløy and Florø.

Geographic entities mentioned:
surface_form: Hornelen
instance_of: Mountain
countries: Norway
coordinates: lat: 61.841666666667
lon: 5.2472222222222
The Utah State Road Commission took over maintenance of State Route 69 from Brigham City via Collinston to Logan on May 12, 1931. The route began at the present SR-13 - then US-30S - in Brigham City, and ran north on the east side of the valley to Collinston. There it turned east over Beaver Dam Summit to the north of the Wellsville Mountains, and crossed the Cache Valley to US-91 in Logan.

Geographic entities mentioned:
surface_form: Cache Valley
instance_of: Valley
countries: United States
coordinates: lat: 41.816666666667
lon: -111.93416666667