Sarmila/GeoWiki-Features huggingface dataset:
Echo Lake is a mountain lake within the Indian Head Wilderness of the Catskill Mountains, located in the valley between the two mountains Plattekill and Overlook, near Woodstock, New York, United States of America. Echo Lake was historically named Shens Lake in state law defining the borders of Ulster County, circa. 1777-1801, or Shoes Lake in the Beer's 1875 Ulster County Atlas. Description.

Geographic entities mentioned:
surface_form: echo lake
instance_of: Lake
countries: United States
coordinates: lat: 44.1753
lon: -71.6922
surface_form: echo lake
instance_of: Lake
countries: United States
coordinates: lat: 48.126666666667
lon: -114.04166666667
surface_form: echo lake
instance_of: Lake
countries: United States
coordinates: lat: 44.8611
lon: -71.9944
surface_form: echo lake
instance_of: Lake
countries: United States
coordinates: lat: 47.771421
lon: -122.343184
surface_form: echo lake
instance_of: Lake
countries: United States
coordinates: lat: 39.658333333333
lon: -105.60333333333
surface_form: echo lake
instance_of: Lake
countries: United States
coordinates: lat: 44.055
lon: -71.1608
surface_form: echo lake
instance_of: Lake
countries: United States
coordinates: lat: 44.438
lon: -70.024
surface_form: echo lake
instance_of: Lake
countries: United States
coordinates: lat: 42.0961
lon: -74.0903
surface_form: echo lake
instance_of: Lake
countries: United States
coordinates: lat: 38.8428
lon: -120.076
surface_form: echo lake
instance_of: Lake
countries: United States
coordinates: lat: 40.6117
lon: -115.447
Description. It carries many species of game fish, fowl, and amphibians. There is a lean-to and seven designated campsites near the lake. Access is by an 8-mile hiking trail, starting around Platte Clove Preserve (County Route 16) up the Old Overlook Road and then around Plattekill Mountain to a junction culminating in a half-mile section called Echo Lake Trail.

Geographic entities mentioned:
surface_form: echo lake
instance_of: Lake
countries: United States
coordinates: lat: 44.1753
lon: -71.6922
surface_form: plattekill mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.107222222222
lon: -74.086666666667
surface_form: echo lake
instance_of: Lake
countries: United States
coordinates: lat: 48.126666666667
lon: -114.04166666667
surface_form: echo lake
instance_of: Lake
countries: United States
coordinates: lat: 44.8611
lon: -71.9944
surface_form: echo lake
instance_of: Lake
countries: United States
coordinates: lat: 47.771421
lon: -122.343184
surface_form: echo lake
instance_of: Lake
countries: United States
coordinates: lat: 39.658333333333
lon: -105.60333333333
surface_form: echo lake
instance_of: Lake
countries: United States
coordinates: lat: 44.055
lon: -71.1608
surface_form: echo lake
instance_of: Lake
countries: United States
coordinates: lat: 44.438
lon: -70.024
surface_form: echo lake
instance_of: Lake
countries: United States
coordinates: lat: 42.0961
lon: -74.0903
surface_form: echo lake
instance_of: Lake
countries: United States
coordinates: lat: 38.8428
lon: -120.076
surface_form: echo lake
instance_of: Lake
countries: United States
coordinates: lat: 40.6117
lon: -115.447
Another route starts at the top of Mead's Mountain in Woodstock, NY; it is quite remote and camping in this spot is backcountry camping, accessible by backpacking only, with no hookups or facilities. Echo Lake is also the Source of the Sawkill River, the main body of water which runs through Woodstock. The psychedelic folk-pop band Woods named their 2009 release, At Echo Lake, in its honor.

Geographic entities mentioned:
surface_form: echo lake
instance_of: Lake
countries: United States
coordinates: lat: 44.1753
lon: -71.6922
surface_form: echo lake
instance_of: Lake
countries: United States
coordinates: lat: 48.126666666667
lon: -114.04166666667
surface_form: echo lake
instance_of: Lake
countries: United States
coordinates: lat: 44.8611
lon: -71.9944
surface_form: echo lake
instance_of: Lake
countries: United States
coordinates: lat: 47.771421
lon: -122.343184
surface_form: echo lake
instance_of: Lake
countries: United States
coordinates: lat: 39.658333333333
lon: -105.60333333333
surface_form: echo lake
instance_of: Lake
countries: United States
coordinates: lat: 44.055
lon: -71.1608
surface_form: echo lake
instance_of: Lake
countries: United States
coordinates: lat: 44.438
lon: -70.024
surface_form: echo lake
instance_of: Lake
countries: United States
coordinates: lat: 42.0961
lon: -74.0903
surface_form: echo lake
instance_of: Lake
countries: United States
coordinates: lat: 38.8428
lon: -120.076
surface_form: echo lake
instance_of: Lake
countries: United States
coordinates: lat: 40.6117
lon: -115.447
South Africa, 1879–1881. In 1879, Prior traveled to Durban to report on the Zulu War which had just broken out. While he missed the events at Isandlwana and Rorke's Drift, he did witness subsequent actions including the final Battle of Ulundi He was also with the group who discovered the body of the Prince Imperial.

Geographic entities mentioned:
surface_form: Isandlwana
instance_of: Mountain
countries: South Africa
coordinates: lat: -28.3589
lon: 30.6528
Geography. Kahlenberg is 484 meters high and lies in the northeastern foothills of the Eastern Alps. The mountain is mostly flysch, which is composed of quartz, limestone, marl, and other conglomerates. East of Kahlenberg is Leopoldsberg; and to the west are Reisenberg, Latisberg, and Hermannskogel. History. Kahlenberg (German: bald mountain) was uninhabited until the 18th century.

Geographic entities mentioned:
surface_form: Leopoldsberg
instance_of: Mountain
countries: Austria
coordinates: lat: 48.2789
lon: 16.3453
surface_form: Hermannskogel
instance_of: Mountain
countries: Austria
coordinates: lat: 48.2707124
lon: 16.2945789
surface_form: hermannskogel
instance_of: Mountain
countries: Austria
coordinates: lat: 48.2707124
lon: 16.2945789
surface_form: leopoldsberg
instance_of: Mountain
countries: Austria
coordinates: lat: 48.2789
lon: 16.3453
In 1628, Ferdinand II acquired the mountain from the Klosterneuburg monastery and called it &quot;Josephsberg&quot; (Joseph's Mountain). Only after Emperor Leopold I renamed the original Kahlenberg (the neighbouring mountain) to Leopoldsberg was the name &quot;Kahlenberg&quot; given to the &quot;Josephsberg&quot;.

Geographic entities mentioned:
surface_form: leopoldsberg
instance_of: Mountain
countries: Austria
coordinates: lat: 48.2789
lon: 16.3453
surface_form: kahlenberg
instance_of: Mountain
countries: Austria
coordinates: lat: 48.2761
lon: 16.3333
surface_form: kahlenberg
instance_of: Mountain
countries: Austria
coordinates: lat: 48.2761
lon: 16.3333
Kahlenberg. The Kahlenberg () is a hill () located in the 19th District of Vienna, Austria (Döbling). General. The Kahlenberg lies in the Vienna Woods and is one of the most popular destinations for day-trips from Vienna, offering a view over the entire city. Parts of Lower Austria can also be seen from &quot;Stefaniewarte&quot; at the peak.

Geographic entities mentioned:
surface_form: kahlenberg
instance_of: Mountain
countries: Austria
coordinates: lat: 48.2761
lon: 16.3333
Transportation==. Kahlenberg can be reached by car or by bus (Bus line 38A) via the picturesque Höhenstraße, part of which is cobblestone. The first Austrian cog railway was built to Kahlenberg in 1872 and 1873 and opened in 1874. It was designed by Carl Maader.

Geographic entities mentioned:
surface_form: kahlenberg
instance_of: Mountain
countries: Austria
coordinates: lat: 48.2761
lon: 16.3333
It was designed by Carl Maader. The track climbed 316 meters over 5.5 km and started from the train station in Nußdorf (today the end station of the tram-line D) and connected through Grinzing and Krapfenwaldl to the Kahlenberg Hotel, which opened in 1872. An average of 180,000 passengers used the train line each year.

Geographic entities mentioned:
surface_form: kahlenberg
instance_of: Mountain
countries: Austria
coordinates: lat: 48.2761
lon: 16.3333
It has one of the most important coalfields of India in nearby areas which are Jharia, Kulti, West Bokaro, East Bokaro and Ramgarh. Geography. Bokaro district consists of undulating uplands on the Chota Nagpur Plateau with the Damodar River cutting a valley right across. It has an average elevation of above mean sea level. The highest hill, Lugu Pahar, rises to a height of.

Geographic entities mentioned:
surface_form: Chota Nagpur Plateau
instance_of: Plateau
countries: India
coordinates: lat: 23
lon: 85
Roche de Smet. Roche de Smet is a mountain summit located in the Athabasca River valley of Jasper National Park in Alberta, Canada. It is situated in the De Smet Range of the Canadian Rockies. It was named in 1896 after Pierre-Jean De Smet. Climate. Based on the Köppen climate classification, Roche de Smet is located in a subarctic climate with cold, snowy winters, and mild summers.

Geographic entities mentioned:
surface_form: athabasca
instance_of: Lake
countries: Canada
coordinates: lat: 59.266666666667
lon: -109.45
surface_form: athabasca
instance_of: Mountain
countries: Canada
coordinates: lat: 52.18055555555556
lon: -117.20166666666667
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: roche de smet
instance_of: Mountain
countries: Canada
coordinates: lat: 53.1344
lon: -118.116
It was named in 1896 after Pierre-Jean De Smet. Climate. Based on the Köppen climate classification, Roche de Smet is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C. Precipitation runoff from Roche de Smet drains into tributaries of the Athabasca River.

Geographic entities mentioned:
surface_form: athabasca
instance_of: Lake
countries: Canada
coordinates: lat: 59.266666666667
lon: -109.45
surface_form: athabasca
instance_of: Mountain
countries: Canada
coordinates: lat: 52.18055555555556
lon: -117.20166666666667
surface_form: roche de smet
instance_of: Mountain
countries: Canada
coordinates: lat: 53.1344
lon: -118.116
Roche de Smet. Roche de Smet is a mountain summit located in the Athabasca River valley of Jasper National Park in Alberta, Canada. It is situated in the De Smet Range of the Canadian Rockies. It was named in 1896 after Pierre-Jean De Smet. Climate. Based on the Köppen climate classification, Roche de Smet is located in a subarctic climate with cold, snowy winters, and mild summers.

Geographic entities mentioned:
surface_form: roche de smet
instance_of: Mountain
countries: Canada
coordinates: lat: 53.1344
lon: -118.116
It was named in 1896 after Pierre-Jean De Smet. Climate. Based on the Köppen climate classification, Roche de Smet is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C. Precipitation runoff from Roche de Smet drains into tributaries of the Athabasca River.

Geographic entities mentioned:
surface_form: roche de smet
instance_of: Mountain
countries: Canada
coordinates: lat: 53.1344
lon: -118.116
It belongs to the Autonomous Region of Castilla y León. Overview. The Sierra de la Cabrera Baja forms a natural boundary with Leon Province in the north, Sierra Segundera with Galicia in the west, and Sierra de la Culebra and Sierra de la Gamoneda with the Bragança District of Portugal in the south and southwest. The comarcas of La Carballeda and Tierra del Pan are to the east.

Geographic entities mentioned:
surface_form: Sierra de la Culebra
instance_of: Mountain
countries: Portugal
Spain
coordinates: lat: 41.89833333
lon: -6.33361111
The comarcas of La Carballeda and Tierra del Pan are to the east. The most famous place in the comarca is the Sanabria Lake (&quot;Lago de Sanabria&quot;), the biggest glacial lake in the Iberian Peninsula, with a surface of which is now within the limits of the Sanabria Lake Natural Park. The lake was declared a Natural Park in 1978. The capital of the comarca is Puebla de Sanabria.

Geographic entities mentioned:
surface_form: Sanabria Lake
instance_of: Lake
countries: Spain
coordinates: lat: 42.1225
lon: -6.71916667
The lake was declared a Natural Park in 1978. The capital of the comarca is Puebla de Sanabria. The Sanabria comarca is one of the few areas of Western Europe with a sizeable population of wild wolves, which live in the Sierra de la Culebra mountain range.

Geographic entities mentioned:
surface_form: Sierra de la Culebra
instance_of: Mountain
countries: Portugal
Spain
coordinates: lat: 41.89833333
lon: -6.33361111
HMS St Lawrence (1814). HMS &quot;St Lawrence&quot; was a 112-gun first-rate ship of the line of the Royal Navy that served on Lake Ontario during the War of 1812. Built on the lake at the Royal Navy dockyard in Kingston, Ontario, she was the only Royal Navy ship of the line ever to be launched and operated entirely in fresh water.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
The ship cost Britain £500,000. The day after the ship's launch, an American fleet under Chauncey appeared off Kingston and offered to battle, which the British declined. The vessel did not put to sea until 16 October, making several trips around Lake Ontario. On 19 October, she was struck by lightning, damaging the mast and killing several of the crew.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
Moving west toward the mountainous interior of the state, the climate becomes markedly colder, the number of cloudy days increases, and winter snowfall amounts are greater. Using the January freezing isotherm, the humid subtropical climate (&quot;Cfa&quot;) only exists in parts of Greater Philadelphia and low-lying areas of the lower Susquehanna Valley from Harrisburg downriver.

Geographic entities mentioned:
surface_form: Susquehanna Valley
instance_of: Valley
countries: United States
coordinates: lat: 41.96666666666667
lon: -75.75
Pennsylvania's hardiness zone ranges from 5a in high-elevation areas to 7b in parts of Delaware and Philadelphia Counties. Precipitation. Western areas of the state, particularly cities near Lake Erie, can receive over of snowfall annually, and the entire state receives an average of of rainfall every year. Floods are more common in March and April than other months of the year. Tropical cyclones.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
Mount Moulton. Mount Moulton is a complex of ice-covered shield volcanoes, standing east of Mount Berlin in the Flood Range, Marie Byrd Land, Antarctica. It is named for Richard S. Moulton, chief dog driver at West Base. The volcano is of Pliocene age and is presently inactive. The Prahl Crags are located on the southern slopes of Mount Moulton and are part of a caldera.

Geographic entities mentioned:
surface_form: Mount Berlin
instance_of: Mountain
coordinates: lat: -76.055
lon: -135.825
surface_form: berlin
instance_of: Mountain
coordinates: lat: -76.055
lon: -135.825
surface_form: mount moulton
instance_of: Mountain
coordinates: lat: -76.05
lon: -135.13333333333
surface_form: moulton
instance_of: Mountain
coordinates: lat: -76.05
lon: -135.13333333333
Moulton, chief dog driver at West Base. The volcano is of Pliocene age and is presently inactive. The Prahl Crags are located on the southern slopes of Mount Moulton and are part of a caldera. There, an exposed area of blue ice can be found; this ice contains tephra layers from mainly neighbouring Mount Berlin volcano and some of the ice is almost half a million years old.

Geographic entities mentioned:
surface_form: Prahl Crags
instance_of: Mountain
coordinates: lat: -76.0667
lon: -134.717
surface_form: southern
instance_of: Mountain
coordinates: lat: -74.2
lon: -76.4667
surface_form: mount moulton
instance_of: Mountain
coordinates: lat: -76.05
lon: -135.13333333333
surface_form: moulton
instance_of: Mountain
coordinates: lat: -76.05
lon: -135.13333333333
Geology and geomorphology. Mount Moulton lies in Marie Byrd Land of Western Antarctica and in the region of the West Antarctic Ice Sheet. It is part of a system of volcanoes including Mount Berlin, Mount Takahe and Mount Waesche as well as of recently active subglacial volcanism. The volcano is named for Richard S.

Geographic entities mentioned:
surface_form: Mount Berlin
instance_of: Mountain
coordinates: lat: -76.055
lon: -135.825
surface_form: Mount Takahe
instance_of: Mountain
coordinates: lat: -76.3
lon: -112.1
surface_form: Mount Waesche
instance_of: Mountain
coordinates: lat: -77.166666666667
lon: -126.9
surface_form: takahe
instance_of: Mountain
coordinates: lat: -76.3
lon: -112.1
surface_form: waesche
instance_of: Mountain
coordinates: lat: -77.166666666667
lon: -126.9
surface_form: active
instance_of: Landform
Body of water
coordinates: lat: -63.4167
lon: -56.1667
surface_form: berlin
instance_of: Mountain
coordinates: lat: -76.055
lon: -135.825
The volcano appears to be of Pliocene age and there is no evidence that it was glaciated during its eruptions. Only a few outcrops of Mount Moulton have been dated and these yield ages of 5.3 million years, with further age estimates of 4.9 – 4.7 million years ago, 5.9 million years ago and 1.04 ± 0.04 million years ago at Gawne Nunatak, which is a parasitic cone.

Geographic entities mentioned:
surface_form: Gawne Nunatak
instance_of: Mountain
coordinates: lat: -76.05
lon: -135.4
surface_form: mount moulton
instance_of: Mountain
coordinates: lat: -76.05
lon: -135.13333333333
surface_form: moulton
instance_of: Mountain
coordinates: lat: -76.05
lon: -135.13333333333
Earthquakes have been recorded at Mount Moulton and are either of volcano-tectonic origin or due to the movement of ice along the flanks of the volcano. The mountain is high, rising about above the ice surface on its northern flank, and located within the Flood Range; Mount Berlin lies across the wide, high-elevation Wells Saddle to the west and Kohler Dome is east of Moulton.

Geographic entities mentioned:
surface_form: Kohler Dome
instance_of: Mountain
coordinates: lat: -76.0333
lon: -134.283
surface_form: berlin
instance_of: Mountain
coordinates: lat: -76.055
lon: -135.825
surface_form: mount berlin
instance_of: Mountain
coordinates: lat: -76.055
lon: -135.825
surface_form: moulton
instance_of: Mountain
coordinates: lat: -76.05
lon: -135.13333333333
The mountain is high, rising about above the ice surface on its northern flank, and located within the Flood Range; Mount Berlin lies across the wide, high-elevation Wells Saddle to the west and Kohler Dome is east of Moulton. Even farther east lie Mount Bursey, Mount Andrus, Mount Kosciuszko and Mount Kauffman, in the Ames Range.

Geographic entities mentioned:
surface_form: Mount Bursey
instance_of: Mountain
coordinates: lat: -76.0167
lon: -132.633
surface_form: Mount Andrus
instance_of: Mountain
coordinates: lat: -75.8
lon: -132.3
surface_form: Mount Kauffman
instance_of: Mountain
coordinates: lat: -75.6167
lon: -132.417
surface_form: andrus
instance_of: Mountain
coordinates: lat: -75.8
lon: -132.3
surface_form: bursey
instance_of: Mountain
coordinates: lat: -76.0167
lon: -132.633
surface_form: kauffman
instance_of: Mountain
coordinates: lat: -75.6167
lon: -132.417
Mount Moulton is formed by a complex of glaciated but largely uneroded shield volcanoes with two or possibly three ice-filled calderas, each of which is about wide. The calderas are apart and located at the Prahl Crags, Britt Peak and potentially Kohler Dome localities.

Geographic entities mentioned:
surface_form: Prahl Crags
instance_of: Mountain
coordinates: lat: -76.0667
lon: -134.717
surface_form: Britt Peak
instance_of: Mountain
coordinates: lat: -76.05
lon: -135.117
surface_form: Kohler Dome
instance_of: Mountain
coordinates: lat: -76.0333
lon: -134.283
The calderas are apart and located at the Prahl Crags, Britt Peak and potentially Kohler Dome localities. Additionally the Prahl Crags – remnants of the former caldera rim – are found south, Gawne Nunatak west, Edwards Spur northeast and the Moulton Icefalls on the northern side of the mountain.

Geographic entities mentioned:
surface_form: Prahl Crags
instance_of: Mountain
coordinates: lat: -76.0667
lon: -134.717
surface_form: Gawne Nunatak
instance_of: Mountain
coordinates: lat: -76.05
lon: -135.4
surface_form: moulton
instance_of: Mountain
coordinates: lat: -76.05
lon: -135.13333333333
Additionally the Prahl Crags – remnants of the former caldera rim – are found south, Gawne Nunatak west, Edwards Spur northeast and the Moulton Icefalls on the northern side of the mountain. The total volume of the complex is about, comparable to that of Mount Shasta in the Cascade Range, and is one of the largest volcanoes in the Flood Range and Ames Range.

Geographic entities mentioned:
surface_form: Mount Shasta
instance_of: Mountain
countries: United States
coordinates: lat: 41.409197222222
lon: -122.19488888889
In addition, recognizable tephra layers are found in this ice and appear to originate from explosive eruptions of volcanoes such as Mount Berlin, Mount Takahe and Mount Waesche, although some may come from parasitic vents of Mount Berlin and Mount Moulton.

Geographic entities mentioned:
surface_form: takahe
instance_of: Mountain
coordinates: lat: -76.3
lon: -112.1
surface_form: mount takahe
instance_of: Mountain
coordinates: lat: -76.3
lon: -112.1
surface_form: waesche
instance_of: Mountain
coordinates: lat: -77.166666666667
lon: -126.9
surface_form: mount waesche
instance_of: Mountain
coordinates: lat: -77.166666666667
lon: -126.9
surface_form: berlin
instance_of: Mountain
coordinates: lat: -76.055
lon: -135.825
surface_form: berlin
instance_of: Mountain
coordinates: lat: -76.055
lon: -135.825
surface_form: mount berlin
instance_of: Mountain
coordinates: lat: -76.055
lon: -135.825
surface_form: mount berlin
instance_of: Mountain
coordinates: lat: -76.055
lon: -135.825
surface_form: mount moulton
instance_of: Mountain
coordinates: lat: -76.05
lon: -135.13333333333
surface_form: moulton
instance_of: Mountain
coordinates: lat: -76.05
lon: -135.13333333333
Furthermore, the appearance of the deposits indicates that the eruptions of Mount Berlin were highly explosive. Most likely they eventually fell onto the ice of Mount Moulton, were incorporated in it and then transported downward to the blue ice field.

Geographic entities mentioned:
surface_form: fell
instance_of: Mountain
coordinates: lat: -73.4333
lon: -62.2667
surface_form: field
instance_of: Mountain
coordinates: lat: -80.88333
lon: 158
surface_form: mount moulton
instance_of: Mountain
coordinates: lat: -76.05
lon: -135.13333333333
surface_form: moulton
instance_of: Mountain
coordinates: lat: -76.05
lon: -135.13333333333
Moulton, chief dog driver of the United States Antarctic Service Expedition; the western end of the Flood Range where Mount Moulton lies was visited by this expedition in December 1940. Other field expeditions took place in 1967–1968, 1977–1978, 1993-1994 and 1999–2000. The volcano appears to be of Pliocene age and there is no evidence that it was glaciated during its eruptions.

Geographic entities mentioned:
surface_form: field
instance_of: Mountain
coordinates: lat: -80.88333
lon: 158
Volcanic rocks found at Mount Moulton include pantellerite, phonolite and trachyte; phenocryst phases found in the pantellerite include aenigmatite, anorthoclase, fayalite, hedenbergite, ilmenite and quartz. Blue ice field. A blue ice field has formed within the caldera of Mount Moulton behind the Prahl Crags, and contains ice almost 500,000 years old.

Geographic entities mentioned:
surface_form: field
instance_of: Mountain
coordinates: lat: -80.88333
lon: 158
Blue ice field. A blue ice field has formed within the caldera of Mount Moulton behind the Prahl Crags, and contains ice almost 500,000 years old. It is the oldest dated ice in West Antarctica and much older than ice found elsewhere in West Antarctic ice cores.

Geographic entities mentioned:
surface_form: field
instance_of: Mountain
coordinates: lat: -80.88333
lon: 158
surface_form: prahl crags
instance_of: Mountain
coordinates: lat: -76.0667
lon: -134.717
surface_form: mount moulton
instance_of: Mountain
coordinates: lat: -76.05
lon: -135.13333333333
surface_form: moulton
instance_of: Mountain
coordinates: lat: -76.05
lon: -135.13333333333
It is the oldest dated ice in West Antarctica and much older than ice found elsewhere in West Antarctic ice cores. Such blue ice fields like those found at Mount Moulton form when glaciers run into an obstacle – in this case the Prahl Crags – and part of the ice starts moving vertically as it undergoes ablation processes like sublimation.

Geographic entities mentioned:
surface_form: prahl crags
instance_of: Mountain
coordinates: lat: -76.0667
lon: -134.717
surface_form: mount moulton
instance_of: Mountain
coordinates: lat: -76.05
lon: -135.13333333333
surface_form: moulton
instance_of: Mountain
coordinates: lat: -76.05
lon: -135.13333333333
The volcano is of Pliocene age and is presently inactive. The Prahl Crags are located on the southern slopes of Mount Moulton and are part of a caldera. There, an exposed area of blue ice can be found; this ice contains tephra layers from mainly neighbouring Mount Berlin volcano and some of the ice is almost half a million years old. Geology and geomorphology.

Geographic entities mentioned:
surface_form: berlin
instance_of: Mountain
coordinates: lat: -76.055
lon: -135.825
surface_form: mount berlin
instance_of: Mountain
coordinates: lat: -76.055
lon: -135.825
Only a few outcrops of Mount Moulton have been dated and these yield ages of 5.3 million years, with further age estimates of 4.9 – 4.7 million years ago, 5.9 million years ago and 1.04 ± 0.04 million years ago at Gawne Nunatak, which is a parasitic cone. There is no evidence of eruptive or thermal activity unlike at its neighbour Mount Berlin.

Geographic entities mentioned:
surface_form: berlin
instance_of: Mountain
coordinates: lat: -76.055
lon: -135.825
surface_form: mount berlin
instance_of: Mountain
coordinates: lat: -76.055
lon: -135.825
These tephra layers at Mount Moulton crop out in parallel layers and geochemical traits indicate an origin at Mount Berlin although some layers may have been erupted from mafic volcanoes at Mount Moulton and Mount Berlin. Furthermore, the appearance of the deposits indicates that the eruptions of Mount Berlin were highly explosive.

Geographic entities mentioned:
surface_form: berlin
instance_of: Mountain
coordinates: lat: -76.055
lon: -135.825
surface_form: berlin
instance_of: Mountain
coordinates: lat: -76.055
lon: -135.825
surface_form: mount berlin
instance_of: Mountain
coordinates: lat: -76.055
lon: -135.825
surface_form: mount berlin
instance_of: Mountain
coordinates: lat: -76.055
lon: -135.825
surface_form: mount moulton
instance_of: Mountain
coordinates: lat: -76.05
lon: -135.13333333333
surface_form: mount moulton
instance_of: Mountain
coordinates: lat: -76.05
lon: -135.13333333333
surface_form: moulton
instance_of: Mountain
coordinates: lat: -76.05
lon: -135.13333333333
surface_form: moulton
instance_of: Mountain
coordinates: lat: -76.05
lon: -135.13333333333
These tephra layers at Mount Moulton crop out in parallel layers and geochemical traits indicate an origin at Mount Berlin although some layers may have been erupted from mafic volcanoes at Mount Moulton and Mount Berlin. Furthermore, the appearance of the deposits indicates that the eruptions of Mount Berlin were highly explosive.

Geographic entities mentioned:
surface_form: berlin
instance_of: Mountain
coordinates: lat: -76.055
lon: -135.825
surface_form: mount berlin
instance_of: Mountain
coordinates: lat: -76.055
lon: -135.825
Mount Moulton. Mount Moulton is a complex of ice-covered shield volcanoes, standing east of Mount Berlin in the Flood Range, Marie Byrd Land, Antarctica. It is named for Richard S. Moulton, chief dog driver at West Base. The volcano is of Pliocene age and is presently inactive. The Prahl Crags are located on the southern slopes of Mount Moulton and are part of a caldera.

Geographic entities mentioned:
surface_form: mount moulton
instance_of: Mountain
coordinates: lat: -76.05
lon: -135.13333333333
surface_form: moulton
instance_of: Mountain
coordinates: lat: -76.05
lon: -135.13333333333
Geology and geomorphology. Mount Moulton lies in Marie Byrd Land of Western Antarctica and in the region of the West Antarctic Ice Sheet. It is part of a system of volcanoes including Mount Berlin, Mount Takahe and Mount Waesche as well as of recently active subglacial volcanism. The volcano is named for Richard S.

Geographic entities mentioned:
surface_form: mount moulton
instance_of: Mountain
coordinates: lat: -76.05
lon: -135.13333333333
surface_form: moulton
instance_of: Mountain
coordinates: lat: -76.05
lon: -135.13333333333
The volcano is named for Richard S. Moulton, chief dog driver of the United States Antarctic Service Expedition; the western end of the Flood Range where Mount Moulton lies was visited by this expedition in December 1940. Other field expeditions took place in 1967–1968, 1977–1978, 1993-1994 and 1999–2000.

Geographic entities mentioned:
surface_form: mount moulton
instance_of: Mountain
coordinates: lat: -76.05
lon: -135.13333333333
surface_form: moulton
instance_of: Mountain
coordinates: lat: -76.05
lon: -135.13333333333
surface_form: moulton
instance_of: Mountain
coordinates: lat: -76.05
lon: -135.13333333333
There is no evidence of eruptive or thermal activity unlike at its neighbour Mount Berlin. Earthquakes have been recorded at Mount Moulton and are either of volcano-tectonic origin or due to the movement of ice along the flanks of the volcano.

Geographic entities mentioned:
surface_form: mount moulton
instance_of: Mountain
coordinates: lat: -76.05
lon: -135.13333333333
surface_form: moulton
instance_of: Mountain
coordinates: lat: -76.05
lon: -135.13333333333
Even farther east lie Mount Bursey, Mount Andrus, Mount Kosciuszko and Mount Kauffman, in the Ames Range. Mount Moulton is an obstacle to ice flow in the West Antarctic Ice Sheet, which has piled up on the mountain and is about higher on the upstream side.

Geographic entities mentioned:
surface_form: mount moulton
instance_of: Mountain
coordinates: lat: -76.05
lon: -135.13333333333
surface_form: moulton
instance_of: Mountain
coordinates: lat: -76.05
lon: -135.13333333333
Mount Moulton is an obstacle to ice flow in the West Antarctic Ice Sheet, which has piled up on the mountain and is about higher on the upstream side. Mount Moulton is formed by a complex of glaciated but largely uneroded shield volcanoes with two or possibly three ice-filled calderas, each of which is about wide.

Geographic entities mentioned:
surface_form: mount moulton
instance_of: Mountain
coordinates: lat: -76.05
lon: -135.13333333333
surface_form: moulton
instance_of: Mountain
coordinates: lat: -76.05
lon: -135.13333333333
The total volume of the complex is about, comparable to that of Mount Shasta in the Cascade Range, and is one of the largest volcanoes in the Flood Range and Ames Range. Only the western part of the Mount Moulton emerges from the ice.

Geographic entities mentioned:
surface_form: mount moulton
instance_of: Mountain
coordinates: lat: -76.05
lon: -135.13333333333
surface_form: moulton
instance_of: Mountain
coordinates: lat: -76.05
lon: -135.13333333333
Only the western part of the Mount Moulton emerges from the ice. Volcanic rocks found at Mount Moulton include pantellerite, phonolite and trachyte; phenocryst phases found in the pantellerite include aenigmatite, anorthoclase, fayalite, hedenbergite, ilmenite and quartz. Blue ice field.

Geographic entities mentioned:
surface_form: mount moulton
instance_of: Mountain
coordinates: lat: -76.05
lon: -135.13333333333
surface_form: moulton
instance_of: Mountain
coordinates: lat: -76.05
lon: -135.13333333333
Such blue ice fields like those found at Mount Moulton form when glaciers run into an obstacle – in this case the Prahl Crags – and part of the ice starts moving vertically as it undergoes ablation processes like sublimation. In the case of Mount Moulton, this outcrop of ice is about long.

Geographic entities mentioned:
surface_form: mount moulton
instance_of: Mountain
coordinates: lat: -76.05
lon: -135.13333333333
surface_form: moulton
instance_of: Mountain
coordinates: lat: -76.05
lon: -135.13333333333
Mount Moulton. Mount Moulton is a complex of ice-covered shield volcanoes, standing east of Mount Berlin in the Flood Range, Marie Byrd Land, Antarctica. It is named for Richard S. Moulton, chief dog driver at West Base. The volcano is of Pliocene age and is presently inactive. The Prahl Crags are located on the southern slopes of Mount Moulton and are part of a caldera.

Geographic entities mentioned:
surface_form: moulton
instance_of: Mountain
coordinates: lat: -76.05
lon: -135.13333333333
Children understood the language, but mostly did not use it. In the late 1990s, the water levels of Lake Vegoritida decreased and new land became exposed for cultivation. The land became the centre of an ownership dispute, involving sometimes violent incidents with the neighbouring village of Agios Panteleimonas.

Geographic entities mentioned:
surface_form: Lake Vegoritida
instance_of: Lake
countries: Greece
coordinates: lat: 40.760555555556
lon: 21.789166666667
Allan Water (Ontario). Allan Water is a river in the James Bay drainage basin in Unorganized Thunder Bay District in northwestern Ontario, Canada. Course. The river begins at the community of Allanwater Bridge at the confluence of the two branches of the Brightsand River: the western branch arriving as the outlet from Kawaweogama Lake and the eastern branch arriving as the outlet from McEwan Lake.

Geographic entities mentioned:
surface_form: Kawaweogama Lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.1994
lon: -90.1861
Shen attracted public attention with the launch of &quot;Funü&quot;; in her newfound capacity as a leading women's rights activist, she attended a women's conference at Mount Lu organized by Soong Mei-ling and thereafter chaired the New Life Movement Women Supervision Committee's cultural affairs group, with an interest in mobilizing female factory workers for the anti-Japanese resistance.

Geographic entities mentioned:
surface_form: Mount Lu
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 29.5725
lon: 115.97333333333
Wylie engaged in the militant action, gave speeches and rallied marches. On 25 July 1910, she was a speaker at Calton Hill, Edinburgh, delivering a synchronized speech that was also being delivered in London about the passing of the women's suffrage bill in its second reading, along with a plea to Parliament to allow the bill to pass into law.

Geographic entities mentioned:
surface_form: Calton Hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 55.955278
lon: -3.182222
Filming for &quot;The 40-Year-Old Virgin&quot; started on January 17, 2005, and wrapped on April 1, 2005. The movie was shot in parts of California, including Studio City, Los Angeles, and San Fernando Valley's Ventura Boulevard. Lyle Workman composed the film's score while Jack N. Green and Brent White respectively served as its cinematographer and editor.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
Christian Sesma is an American filmmaker. He has directed such films as &quot;Vigilante Diaries&quot; (2016), &quot;Paydirt&quot; (2020), &quot;Take Back&quot; (2021) and &quot;Every Last One of Them&quot; (2021). Sesma was born and raised in the Coachella Valley. He grew up in Palm Springs, California. He divides his time between Cathedral City, California and West Hollywood, California.

Geographic entities mentioned:
surface_form: Coachella Valley
instance_of: Valley
countries: United States
coordinates: lat: 33.72
lon: -116.2
The neighborhood is bounded on the north by Lakewood Gulch, on the east by Federal Boulevard, on the south by the 6th Avenue Freeway, and on the west by Sheridan Boulevard, except for a small notch occupying a few square blocks that protrudes to the westward of Sheridan Boulevard between 10th Avenue and Lakewood Gulch.

Geographic entities mentioned:
surface_form: Lakewood Gulch
instance_of: Landform
countries: United States
coordinates: lat: 39.7378
lon: -105.022
Schluchsee. The Schluchsee () is a reservoir lake in the district of Breisgau-Hochschwarzwald, southeast of the Titisee in the Black Forest near Freiburg im Breisgau, Germany. Name. In the Alemannic dialects of the region the name of the lake is the &quot;Schluechs&quot; or &quot;Schlues&quot;.

Geographic entities mentioned:
surface_form: Titisee
instance_of: Lake
countries: Germany
coordinates: lat: 47.893333333333
lon: 8.1461111111111
The Minas Basin is divided into four sections: (1) the Minas Channel, from the shortest line between Cape Chignecto and the Annapolis Valley Shore to Minas Passage, between Parrsboro and Cape Blomidon; (2) Central Minas Basin, from Minas Passage to the mouth of Cobequid Bay, the shortest line point between Economy and the Noel Shore; (3) Cobequid Bay which extends to the mouth of the Salmon River; and (4) the Southern Bight, from the mouth of the Avon River to the shortest line between Cape Blomidon and the Noel Shore.

Geographic entities mentioned:
surface_form: Annapolis Valley
instance_of: Valley
countries: Canada
coordinates: lat: 44.979166666666664
lon: -64.89222222222222
Several large rivers drain into the Minas Basin: the Shubenacadie River, Cornwallis River, Avon River, Gaspereau River, and Salmon River. Lesser rivers include the Canard River, Diligent River, Farrell River, and the Debert River. Along the northern edge of the Minas Basin lies a chain of intermittent high-cliffed basaltic bluffs and islands called the Basalt Headlands.

Geographic entities mentioned:
surface_form: Canard River
instance_of: Watercourse
countries: Canada
coordinates: lat: 45.1226
lon: -64.4355
Berardo dei Marsi was born in 1079 to Berardo and Theodosia. He was the great-uncle of Saint Rosalia. As a child he studied with the canons of the cathedral of Santa Sabina dei Marsi and also studied at Monte Cassino from 1095 to 1102. He became the governor of Campagna after Pope Paschal II appointed him to that position. He also served as an administrator to Campagna at the behest of the pope.

Geographic entities mentioned:
surface_form: Monte Cassino
instance_of: Mountain
countries: Italy
coordinates: lat: 41.49
lon: 13.813888888889
Called the Lubusz Land while part of medieval Poland, the territory later known as the Neumark gradually became part of the German Margraviate of Brandenburg from the mid-13th century.

Geographic entities mentioned:
surface_form: Lubusz Land
instance_of: Plateau
countries: Germany
Poland
Kingdom of Poland
Lands of the Bohemian Crown
Middle Ages. The region came under the sovereignty of the first Polish state during the 10th-century rule of Mieszko I (died 992) and Bolesław I (ruled 992–1025), Dukes of the Polans. Polish rulers incorporated the future Neumark territory as the Lubusz Land and by the beginning of the 13th century the previously depopulated region had a thinly-spread population of Poles.

Geographic entities mentioned:
surface_form: Lubusz Land
instance_of: Plateau
countries: Germany
Poland
Kingdom of Poland
Lands of the Bohemian Crown
Its namesake was the county of Northamptonshire in England, and the county seat of Easton was named for Easton Neston, a country house in Northamptonshire. Northampton County and Lehigh County to its west combine to form the eastern Pennsylvania region known as the Lehigh Valley; Lehigh County, with a population of 374,557 as of the 2020 U.S.

Geographic entities mentioned:
surface_form: Lehigh Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.7
lon: -75.5
10.5% of the population were of Hispanic or Latino ancestry. Economy. Northampton County is part of the larger Lehigh Valley metropolitan region, which was historically a global leader in heavy manufacturing. As of 2023, the Lehigh Valley's gross domestic product (GDP) was $ billion, led by its manufacturing sector, which comprised $9 billion, or 16 percent.

Geographic entities mentioned:
surface_form: Lehigh Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.7
lon: -75.5
Rosemead, California. Rosemead is a city in Los Angeles County, California, United States. The 2020 United States census reported a population of 51,185. Rosemead is part of a cluster of cities, along with Alhambra, Arcadia, Temple City, Monterey Park, San Marino, and San Gabriel, in the west San Gabriel Valley with a growing Asian-American population. History.

Geographic entities mentioned:
surface_form: San Gabriel Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.101944444444
lon: -118.10277777778
The ranch was later transferred to Juan Matias Sánchez. In 1852, John and Harriet Guess moved cross-country in an ox drawn wagon, to the San Gabriel Valley from Conway County, Arkansas. In 1855, the couple camped where present-day Savannah Elementary School is located on Rio Hondo Avenue. They rented the land until 1867, when John Guess purchased of a ranch and named it Savannah.

Geographic entities mentioned:
surface_form: San Gabriel Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.101944444444
lon: -118.10277777778
It was named Flair Park and the roadway that parallels I-10 was named Flair Drive. Demographics. Rosemead is part of a cluster of cities (along with Arcadia, Temple City, Monterey Park, San Marino, and San Gabriel) in the west San Gabriel Valley with a growing Asian population. Rosemead has a significant population from Mexico, among other Latino nationalities.

Geographic entities mentioned:
surface_form: San Gabriel Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.101944444444
lon: -118.10277777778
The decline of the huia over the southern half of the North Island occurred at markedly different rates in different locations. Areas where dramatic declines were observed in the 1880s included the Puketoi Range, the Hutt Valley and Tararuas, and the Pahiatua-Dannevirke area.

Geographic entities mentioned:
surface_form: Hutt Valley
instance_of: Valley
countries: New Zealand
coordinates: lat: -41.1657
lon: 174.973
Sightings of the huia were also reported there in 1912 and 1913. Despite this, naturalists from the Dominion Museum in Wellington did not investigate the reports. The last credible reports of huia come from the forests of Te Urewera National Park, with one from near Mt Urutawa in 1952 and final sightings near Lake Waikareiti in 1961 and 1963.

Geographic entities mentioned:
surface_form: Lake Waikareiti
instance_of: Lake
countries: New Zealand
coordinates: lat: -38.715
lon: 177.169
It has an altitude of and is located in the territory of Bílina in the Ústí nad Labem Region. When seen from the northwest side, the hill has the shape of a lying lion. It is a structure similar to the Devils Tower in Wyoming, and is the largest phonolite structure of its kind in Europe. There are also mineral water springs which are the source of Bílinská Kyselka water.

Geographic entities mentioned:
surface_form: Devils Tower
instance_of: Mountain
countries: United States
coordinates: lat: 44.590277777778
lon: -104.71527777778
Bořeň. Bořeň () is a phonolite hill in the Central Bohemian Uplands in the Czech Republic. It has an altitude of and is located in the territory of Bílina in the Ústí nad Labem Region. When seen from the northwest side, the hill has the shape of a lying lion. It is a structure similar to the Devils Tower in Wyoming, and is the largest phonolite structure of its kind in Europe.

Geographic entities mentioned:
surface_form: bořeň
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.5276581
lon: 13.7639003
Willow Lake (Idaho). Willow Lake is an alpine lake in Custer County, Idaho, United States, located in the White Cloud Mountains in the Sawtooth National Recreation Area. The lake is accessed from Sawtooth National Forest trail 683. Willow Lake is northeast of Merriam Peak and located in the lower section of the Boulder Chain Lakes Basin.

Geographic entities mentioned:
surface_form: Boulder Chain Lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 44.0704685
lon: -114.5835292
In recent history, this phenomenon has been observed twice. The first recorded limnic eruption occurred in Cameroon at Lake Monoun in 1984, causing asphyxiation and death of 37 people living nearby. A second, deadlier eruption happened at neighboring Lake Nyos in 1986, releasing over 80 million m3 of, killing around 1,700 people and 3,000 livestock, again by asphyxiation.

Geographic entities mentioned:
surface_form: Lake Nyos
instance_of: Lake
countries: Cameroon
coordinates: lat: 6.4380555555556
lon: 10.298888888889
A second, deadlier eruption happened at neighboring Lake Nyos in 1986, releasing over 80 million m3 of, killing around 1,700 people and 3,000 livestock, again by asphyxiation. A third lake, the much larger Lake Kivu, rests on the border between the Democratic Republic of the Congo and Rwanda, and contains massive amounts of dissolved.

Geographic entities mentioned:
surface_form: Lake Kivu
instance_of: Lake
countries: Democratic Republic of the Congo
Rwanda
coordinates: lat: -1.8530555555556
lon: 29.135277777778
Degassing. Efforts are underway to develop a solution for removing the gas from these lakes and to prevent a build-up which could lead to another disaster. A team led by French scientist Michel Halbwachs began experimenting at Lake Monoun and Lake Nyos in 1990 using siphons to degas the waters of these lakes in a controlled manner.

Geographic entities mentioned:
surface_form: Lake Nyos
instance_of: Lake
countries: Cameroon
coordinates: lat: 6.4380555555556
lon: 10.298888888889
In January 2003, an 18-month project was approved to fully degas Lake Monoun, and the lake has since been rendered safe. There is some evidence that Lake Michigan in the United States spontaneously degasses on a much smaller scale each fall. Lake Kivu risks.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Lake Kivu risks. Lake Kivu is not only about 1,700 times larger than Lake Nyos, but is also located in a far more densely populated area, with over two million people living along its shores. The part within the Democratic Republic of the Congo is a site of active armed conflict and low state capacity for the DRC government, which impedes both studies and any subsequent mitigating actions.

Geographic entities mentioned:
surface_form: Lake Kivu
instance_of: Lake
countries: Democratic Republic of the Congo
Rwanda
coordinates: lat: -1.8530555555556
lon: 29.135277777778
surface_form: Lake Nyos
instance_of: Lake
countries: Cameroon
coordinates: lat: 6.4380555555556
lon: 10.298888888889
The area, nearby cities. Jahu is an emerging small town. The nearest major town is Sarkaghat. Bhota is west, and Jahu is east of Hamipur, and from Shimla,
To the north, is Palampur, to the east, is Rewalsar Lake (see also Rewalsar, India), and to the west is Hoshiarpur. Jahu Khurd is south. Big cities close to Jahu are Hamirpur, west, Sundarnagar at, Mandi at, and Nangal at.

Geographic entities mentioned:
surface_form: Rewalsar Lake
instance_of: Lake
countries: India
coordinates: lat: 31.633888888889
lon: 76.833330555556
Kangana Ranaut, a Bollywood actress, did her primary education in Bhambla near Jahu. The Area. Jahu is near Gobind Sagar, a reservoir on the Sutlej river, which flows south of town. The Beas Satluj Link Project is northeast, as is Prashar Lake. The confluence of the Sunail Khad and the Seer Khad is just south of Jahu. The Sunail Khad flows west of Jahu. The Seer Khad flows into the Sutlej.

Geographic entities mentioned:
surface_form: Prashar Lake
instance_of: Lake
countries: India
coordinates: lat: 31.754261111111
lon: 77.101411111111