Sarmila/GeoWiki-Features huggingface dataset:
At the end of this eruptive sequence, rhyodacite lava domes formed on the northeastern slopes of the volcano. Between 100 and 200 years before the climactic eruption, Llao Rock, a thick block of dark lava with a volume of, was produced from a rhyodacite flow erupted from Mazama. It has a round center and extensions on the sides, resembling a bird of prey.

Geographic entities mentioned:
surface_form: mazama
instance_of: Mountain
countries: United States
coordinates: lat: 42.9165186
lon: -122.0844711
A large crater formed but was filled by subsequent lava flows. Shortly before the major, caldera-forming eruption at Mazama, the Cleetwood flow was produced. Also composed of rhyodacite lava, it originated from a vent on the northern side of the complex eastward of Llao Rock.

Geographic entities mentioned:
surface_form: mazama
instance_of: Mountain
countries: United States
coordinates: lat: 42.9165186
lon: -122.0844711
Also composed of rhyodacite lava, it originated from a vent on the northern side of the complex eastward of Llao Rock. It likely only occurred weeks or months before the major eruption, as Mazama's collapse formed a backward flow of lava when it cut through the Cleetwood lava, suggesting that the Cleetwood lava was still hot enough to flow and move.

Geographic entities mentioned:
surface_form: mazama
instance_of: Mountain
countries: United States
coordinates: lat: 42.9165186
lon: -122.0844711
Tephra from the last major eruption that was emplaced atop Cleetwood deposits has been altered by heat and gas from the Cleetwood lava. Both these eruptive periods took place on the northern flank of the Mazama complex, not far from the magma chamber that produced the climactic eruption shortly after. Climactic eruption.

Geographic entities mentioned:
surface_form: mazama
instance_of: Mountain
countries: United States
coordinates: lat: 42.9165186
lon: -122.0844711
Fallout from the eruption continued for roughly three years, though the major eruption only occurred for a few days. The eruption is thought to have occurred during autumn, as inferred from pollen data. The eruptive activity that led to Mazama's collapse proceeded in two phases.

Geographic entities mentioned:
surface_form: mazama
instance_of: Mountain
countries: United States
coordinates: lat: 42.9165186
lon: -122.0844711
The eruptive activity that led to Mazama's collapse proceeded in two phases. During the first phase, shortly after the eruption of the &quot;Cleetwood flow&quot;, a vent at a higher elevation on the northern side of the Mazama complex (but still below the summit) produced a high ash column into the stratosphere and ejecting over half the eruption's total magma.

Geographic entities mentioned:
surface_form: mazama
instance_of: Mountain
countries: United States
coordinates: lat: 42.9165186
lon: -122.0844711
The second stage erupted material from a ring of vents. Ash extended to eight states in the west and three Canadian provinces. As a result, Mazama Ash has become a commonly used benchmark for measuring the relative age of objects, compared to its orange colored deposits. Pumice deposits reached depths of adjacent to Mazama's base, still reaching thicknesses more than as far as to the northeast.

Geographic entities mentioned:
surface_form: mazama
instance_of: Mountain
countries: United States
coordinates: lat: 42.9165186
lon: -122.0844711
Ashfall layers have been eroded by pyroclastic flows and with time, but they are still visible at Hillman Peak and along the Cleetwood Trail. The Plinian column from the eruption devastated the area hundreds of miles north and northeast of Mazama, but to the southwest and west, little pumice or ash were deposited.

Geographic entities mentioned:
surface_form: mazama
instance_of: Mountain
countries: United States
coordinates: lat: 42.9165186
lon: -122.0844711
Eventually, the top of Mazama's magma chamber subsided, and concentric openings formed by the summit, producing smaller vents surrounding the main eruptive cone. Pumice ejected from these new fractures created rapid pyroclastic flows that coursed down all the sides of Mazama, traveling over tall ridges and summits of subfeatures and extending tens of miles from their vents.

Geographic entities mentioned:
surface_form: mazama
instance_of: Mountain
countries: United States
coordinates: lat: 42.9165186
lon: -122.0844711
Pumice ejected from these new fractures created rapid pyroclastic flows that coursed down all the sides of Mazama, traveling over tall ridges and summits of subfeatures and extending tens of miles from their vents. These flows altered the surfaces surrounding Mazama, removing ashfall and then depositing their contents in nearby valleys.

Geographic entities mentioned:
surface_form: mazama
instance_of: Mountain
countries: United States
coordinates: lat: 42.9165186
lon: -122.0844711
These flows altered the surfaces surrounding Mazama, removing ashfall and then depositing their contents in nearby valleys. Some of the flows traveled more than from their source, destroying timber in their paths, while others deposited their rock into river valleys to the north and west of Mazama, leaving layers of pumice between in thickness. Ash clouds also rose up from the pyroclastic flows.

Geographic entities mentioned:
surface_form: mazama
instance_of: Mountain
countries: United States
coordinates: lat: 42.9165186
lon: -122.0844711
Ash clouds also rose up from the pyroclastic flows. Pyroclastic flows also moved to the east, reaching more than from the base of Mazama. These deposits have diameters between, though they are punctuated by pumice blocks with diameters of that extend as far as from Mazama's summit.

Geographic entities mentioned:
surface_form: mazama
instance_of: Mountain
countries: United States
coordinates: lat: 42.9165186
lon: -122.0844711
These deposits have diameters between, though they are punctuated by pumice blocks with diameters of that extend as far as from Mazama's summit. Flows containing pumice coursed into the Annie Creek and Sun Creek canyons southward of Mazama, depositing of material, which have still not been fully eroded after almost 8,000 years.

Geographic entities mentioned:
surface_form: mazama
instance_of: Mountain
countries: United States
coordinates: lat: 42.9165186
lon: -122.0844711
The last of the pyroclastic flows erupted contained andesitic, gray scoria that was deposited above the pale orange and yellow rhyodacite pumice from earlier phases of the eruption. The final eruptions formed the Pumice Desert, a treeless plain on the northern and northeastern side of Mazama, as well as filling the Pumice Creek valley and parts of the Klamath Marsh.

Geographic entities mentioned:
surface_form: mazama
instance_of: Mountain
countries: United States
coordinates: lat: 42.9165186
lon: -122.0844711
Erosion from rain and stream flow has left pipes from the andesitic lava flows as columns and spires. Before collapse due to eruption of magma emptying the underlying magma chamber, the Mazama edifice had an estimated volume of, though it may have exceeded taking glacial erosion into account.

Geographic entities mentioned:
surface_form: mazama
instance_of: Mountain
countries: United States
coordinates: lat: 42.9165186
lon: -122.0844711
Before collapse due to eruption of magma emptying the underlying magma chamber, the Mazama edifice had an estimated volume of, though it may have exceeded taking glacial erosion into account. After the climactic eruption, Mazama's peak was completely destroyed, replaced by a depression with a depth of surrounded by cliffs.

Geographic entities mentioned:
surface_form: mazama
instance_of: Mountain
countries: United States
coordinates: lat: 42.9165186
lon: -122.0844711
After the climactic eruption, Mazama's peak was completely destroyed, replaced by a depression with a depth of surrounded by cliffs. The volume of magma erupted from Mazama during this eruption was 14 cubic miles (61 km3). The lava produced was zoned vertically according to arrangement within the source magma chamber, and was calc-alkaline in composition.

Geographic entities mentioned:
surface_form: mazama
instance_of: Mountain
countries: United States
coordinates: lat: 42.9165186
lon: -122.0844711
Mazama's climactic eruption was one of the largest eruptions during the Holocene epoch. Considering Mazama's eruptive output within the past 420,000 years, it may have produced more than of eruptive volume, making it either the third or fourth most productive Quaternary volcanic center in the Cascade Range.

Geographic entities mentioned:
surface_form: mazama
instance_of: Mountain
countries: United States
coordinates: lat: 42.9165186
lon: -122.0844711
It forms orange colored deposits. Like the Glacier Peak Ash deposits, Mazama Ash is well preserved in the Pacific Northwest. It is distinguishable from the lump pumice deposits ejected from the Glacier Peak volcano, which contain more phenocrysts.

Geographic entities mentioned:
surface_form: mazama
instance_of: Mountain
countries: United States
coordinates: lat: 42.9165186
lon: -122.0844711
Recent activity and potential hazards. Since the climactic eruption 7,700 years ago, all eruptive activity at Mazama has occurred within the caldera. After the caldera formed, the original crater was widened by avalanches from the walls. These gave a scalloped profile to the caldera, such as the coves at Llao Bay, Steel Bay, and Grotto Cove.

Geographic entities mentioned:
surface_form: mazama
instance_of: Mountain
countries: United States
coordinates: lat: 42.9165186
lon: -122.0844711
This eruption took place underwater, and it produced viscous lava that created a rhyodacite lava dome, about 2,400 years after the first period of postcaldera activity. Given that Mazama has had periods of sporadic eruptions for 420,000 years, the United States Geological Survey thinks that it is &quot;virtually certain&quot; that Mazama will erupt again in the future.

Geographic entities mentioned:
surface_form: mazama
instance_of: Mountain
countries: United States
coordinates: lat: 42.9165186
lon: -122.0844711
surface_form: mazama
instance_of: Mountain
countries: United States
coordinates: lat: 42.9165186
lon: -122.0844711
Eruptions are unlikely to produce waves that extend beyond Crater Lake, but powerful explosions could produce tall waves in the caldera. An eruption as explosive as the one 7,700 years ago is unlikely given that it would require larger volumes of magma than are known to be available within the Mazama vicinity.

Geographic entities mentioned:
surface_form: mazama
instance_of: Mountain
countries: United States
coordinates: lat: 42.9165186
lon: -122.0844711
Though the population within of Mount Mazama is only about 50 people, more than 270,000 live within of the volcano. Even so, highly consequential eruptions at Mazama seem unlikely in the near future. Large, pyroclastic eruptions like the climactic eruption are unlikely for thousands of years.

Geographic entities mentioned:
surface_form: mazama
instance_of: Mountain
countries: United States
coordinates: lat: 42.9165186
lon: -122.0844711
Most springs show similar chemistry, from the weathering of volcanic glass and clinopyroxene. These features probably formed due to processes related to residual heat from the magma chamber that produced the climactic Mazama eruption 7,700 years ago.

Geographic entities mentioned:
surface_form: mazama
instance_of: Mountain
countries: United States
coordinates: lat: 42.9165186
lon: -122.0844711
Native American people have lived in the area near Mazama for at least 10,000 years. At least part of the surrounding vicinity was occupied by indigenous populations when Mazama resumed activity about 8,000 years ago, following about 20,000 years of dormancy. Most evidence suggests that Mazama served as a camp site, but not a permanent place of habitation.

Geographic entities mentioned:
surface_form: mazama
instance_of: Mountain
countries: United States
coordinates: lat: 42.9165186
lon: -122.0844711
surface_form: mazama
instance_of: Mountain
countries: United States
coordinates: lat: 42.9165186
lon: -122.0844711
Native populations did not tell settlers about the area because it held sacred importance among tribes throughout Oregon and northern California. Shamans did not allow local Native Americans to look towards Crater Lake, and the Klamath people believed that just looking at Mazama would cause death. Some Native Americans still refuse to look at the water.

Geographic entities mentioned:
surface_form: mazama
instance_of: Mountain
countries: United States
coordinates: lat: 42.9165186
lon: -122.0844711
Geologists had not discovered this mechanism for caldera formation yet, but the hypothesis was recorded by the soldier William M. Colvig in 1865, and then reprinted in Ella Clark's &quot;Indian Legends of the Pacific Northwest&quot;. The last major volcanic landform in the Cascade Range identified by white settlers, Mazama was first visited by non-indigenous people in the spring of 1853.

Geographic entities mentioned:
surface_form: mazama
instance_of: Mountain
countries: United States
coordinates: lat: 42.9165186
lon: -122.0844711
At the time of its collapse, Mount Mazama encompassed an area of and represented one of the major volcanoes in the High Cascades branch of the greater Cascade Range. It was the largest volcanic edifice between Mount Shasta in California and the Three Sisters complex in Oregon.

Geographic entities mentioned:
surface_form: three sisters
instance_of: Mountain
countries: United States
coordinates: lat: 34.5968
lon: -83.9444
surface_form: three sisters
instance_of: Landform
countries: United States
coordinates: lat: 41.7446
lon: -121.473
surface_form: shasta
instance_of: Mountain
countries: United States
coordinates: lat: 41.409197222222
lon: -122.19488888889
surface_form: mount shasta
instance_of: Mountain
countries: United States
coordinates: lat: 41.409197222222
lon: -122.19488888889
surface_form: three sisters
instance_of: Mountain
countries: United States
coordinates: lat: 33.8697
lon: -117.359
By 1992, Crater Lake National Park initiated a bull trout conservation project, removing invasive fish populations with electrofishing, snorkeling, and introduction of the toxin and inhibitor of cellular respiration antimycin A. They also created small barriers to keep new trout from reaching Sun Creek.

Geographic entities mentioned:
surface_form: bull
instance_of: Watercourse
countries: United States
coordinates: lat: 49.46663
lon: -115.45205
They also created small barriers to keep new trout from reaching Sun Creek. In 1999, Bull trout were considered a &quot;threatened&quot; species by the Endangered Species Act, though locally, there are now about 2,000 Bull trout in the stream, almost ten times as many as the low point for Bull trout abundance at just 200 fish.

Geographic entities mentioned:
surface_form: bull
instance_of: Watercourse
countries: United States
coordinates: lat: 49.46663
lon: -115.45205
surface_form: bull
instance_of: Watercourse
countries: United States
coordinates: lat: 49.46663
lon: -115.45205
The project now works with the state government to expand Bull trout distributions from Sun Creek into neighboring forests with fish barriers and removal of invasive fish species. Climate change threatens the American pika populations in the Crater Lake area, as they cannot tolerate warm weather because their fur does not release heat efficiently.

Geographic entities mentioned:
surface_form: bull
instance_of: Watercourse
countries: United States
coordinates: lat: 49.46663
lon: -115.45205
Whenever eruptions took place in the presence of ice, lava was chilled by glaciers, creating glassy talus deposits. Sometimes, the lava coursed into areas previously carved by glaciers like at Sentinel Rock, filling canyons with volcanic rock. Moraines occur up to from the rim of Mazama's caldera, and there are glacial striations visible at several sites in the area.

Geographic entities mentioned:
surface_form: sentinel rock
instance_of: Mountain
countries: United States
coordinates: lat: 37.7288
lon: -119.594
Lousberg. At 264 meters, the Lousberg (historically sometimes also spelled &quot;Louisberg&quot;, &quot;Luisberg&quot; or &quot;Loysberg&quot;) is a prominent elevation on the northern edge of the historic center of Aachen, which was laid out as a forest and mountain park at the beginning of the 19th century according to plans by. The origin of the name is not entirely clear.

Geographic entities mentioned:
surface_form: lousberg
instance_of: Mountain
countries: Germany
coordinates: lat: 50.7869
lon: 6.07917
It was formed during the Upper Cretaceous, when the region around Aachen was affected by a Europe-wide marine transgression, during which initially sandy and later predominantly calcareous sediments were deposited (Aachen Formation). The morphological elevation of the Lousberg is related to the tectonic movements that led to the formation of the Lower Rhine Bight.

Geographic entities mentioned:
surface_form: lousberg
instance_of: Mountain
countries: Germany
coordinates: lat: 50.7869
lon: 6.07917
Silicified wood, charcoal, and numerous concretions of marcasite are embedded in these layers. Due to the water-storing properties of the deposits, the clay of the Hergenrath layers forms the most important spring horizon in the region, both on the Lousberg and in the Aachen Forest.

Geographic entities mentioned:
surface_form: lousberg
instance_of: Mountain
countries: Germany
coordinates: lat: 50.7869
lon: 6.07917
Subsequently, during the Upper Cretaceous, the area was gradually submerged by the sea, and 30–50 m thick quartz sands of the Aachen Formation were deposited, which were mined in small sand pits on the lower slopes of the Lousberg (e.g. at the present playground at the end of).

Geographic entities mentioned:
surface_form: lousberg
instance_of: Mountain
countries: Germany
coordinates: lat: 50.7869
lon: 6.07917
Because of their greenish-brown weathering color, these beds were formerly known as the &quot;Vaals Green Sands&quot;. In the Campanian, tectonic movements began to increase, which are associated with the sinking of the Lower Rhine Bight and led to the uplift of the Lousberg Floe. The Vijlen and limestones were probably not primarily sedimented due to their high altitude.

Geographic entities mentioned:
surface_form: lousberg
instance_of: Mountain
countries: Germany
coordinates: lat: 50.7869
lon: 6.07917
History. During the Neolithic period, about to years ago, flint was mined and worked intensively on the Lousberg. This gray flint, easily recognizable by its characteristic chocolate-brown color zones, was used to make axes and other tools, most of which were polished on-site or brought to settlements as semi-finished products.

Geographic entities mentioned:
surface_form: lousberg
instance_of: Mountain
countries: Germany
coordinates: lat: 50.7869
lon: 6.07917
This gray flint, easily recognizable by its characteristic chocolate-brown color zones, was used to make axes and other tools, most of which were polished on-site or brought to settlements as semi-finished products. The striking coloration of the Lousberg flint makes it a suitable object for studying the distribution of axe blades.

Geographic entities mentioned:
surface_form: lousberg
instance_of: Mountain
countries: Germany
coordinates: lat: 50.7869
lon: 6.07917
The 14C dates of the artifacts found in the Lousberg overburden indicate that the mine was in operation between 3500 and 3000 B.C. Calculations based on the volume of the overburden, the weight of the production waste, and the average weight of the axe blades suggest that about axe blanks left the Lousberg.

Geographic entities mentioned:
surface_form: lousberg
instance_of: Mountain
countries: Germany
coordinates: lat: 50.7869
lon: 6.07917
During the Roman occupation, the limestone was used to build the thermal baths of Aachen, and in the Middle Ages, it was used in the construction of Barbarossa's Wall. At the beginning of the 19th century, the Napoleonic geographer Jean Joseph Tranchot began the topographic survey of the Rhineland at the scale of 1:, starting from a triangulation point on the Lousberg.

Geographic entities mentioned:
surface_form: lousberg
instance_of: Mountain
countries: Germany
coordinates: lat: 50.7869
lon: 6.07917
The inscription praising Napoleon was replaced by the inscription that can still be read today. The damage to the edges of the stone was compensated by chamfering, which is untypical for an obelisk. It was at this time that the first landscape park in Europe, initiated by citizens (and not by princes), was created on the Lousberg.

Geographic entities mentioned:
surface_form: lousberg
instance_of: Mountain
countries: Germany
coordinates: lat: 50.7869
lon: 6.07917
The idea of planting the Lousberg is said to have originated in 1806 and to have been promoted by Johann Wilhelm Körfgen (1769–1829), secretary general of the prefecture of the &quot;département&quot; of Roer. The idea of a park on the Lousberg was combined with the idea of building a society house called the &quot;Belvédère&quot; on the southeastern slope of the mountain.

Geographic entities mentioned:
surface_form: lousberg
instance_of: Mountain
countries: Germany
coordinates: lat: 50.7869
lon: 6.07917
The course itself was also dramatically designed by Weyhe, with flat sections alternating with climbs of varying lengths. Between 1803 and 1814, General Secretary Johann Wilhelm Körfgen had his &quot;Müsch&quot; estate, located on the northern flank of the Lousberg in the Soers, transformed into a &quot;ferme ornée&quot; according to Maximilian Friedrich Weyhe's plans for the Lousberg.

Geographic entities mentioned:
surface_form: lousberg
instance_of: Mountain
countries: Germany
coordinates: lat: 50.7869
lon: 6.07917
At the end of the 19th century, according to the plans of Aachen's director of gardens Heinrich Grube, the park areas of the Lousberg were extended eastwards to include the areas of the Salvatorberg, so that a network of green spaces could be created with the city fortifications (northern parts of the ring of avenues) planned by Maximilian Friedrich Weyhe from 1807 and with today's municipal gardens designed by Peter Joseph Lenné in 1852.

Geographic entities mentioned:
surface_form: lousberg
instance_of: Mountain
countries: Germany
coordinates: lat: 50.7869
lon: 6.07917
In 1906, the city of Aachen rebuilt the Kersten Pavilion, a baroque building designed by the Aachen architect Johann Joseph Couven, on the Lousberg. The pavilion, which is about 100 years older than the Lousberg Park, was previously located in the city of Aachen at Annuntiatenbach 22–28 and was part of the city palace of the wealthy dye-works owner Nicolaus Mantels.

Geographic entities mentioned:
surface_form: lousberg
instance_of: Mountain
countries: Germany
coordinates: lat: 50.7869
lon: 6.07917
In 1906, the city of Aachen rebuilt the Kersten Pavilion, a baroque building designed by the Aachen architect Johann Joseph Couven, on the Lousberg. The pavilion, which is about 100 years older than the Lousberg Park, was previously located in the city of Aachen at Annuntiatenbach 22–28 and was part of the city palace of the wealthy dye-works owner Nicolaus Mantels.

Geographic entities mentioned:
surface_form: lousberg
instance_of: Mountain
countries: Germany
coordinates: lat: 50.7869
lon: 6.07917
surface_form: lousberg
instance_of: Mountain
countries: Germany
coordinates: lat: 50.7869
lon: 6.07917
The pavilion, which is about 100 years older than the Lousberg Park, was previously located in the city of Aachen at Annuntiatenbach 22–28 and was part of the city palace of the wealthy dye-works owner Nicolaus Mantels. To save the building from demolition, the city bought it and had it rebuilt on the Lousberg.

Geographic entities mentioned:
surface_form: lousberg
instance_of: Mountain
countries: Germany
coordinates: lat: 50.7869
lon: 6.07917
The café was known for its 360° panoramic view and the automatic movement of tables around the circular area using a slow conveyor belt. A restaurant has since opened in the same space. Today, the Lousberg is largely wooded and serves as a local recreation area. The extensive park of the former St. Raphael Monastery north of the Lousberg was integrated into the Lousberg Park in 2009.

Geographic entities mentioned:
surface_form: lousberg
instance_of: Mountain
countries: Germany
coordinates: lat: 50.7869
lon: 6.07917
A restaurant has since opened in the same space. Today, the Lousberg is largely wooded and serves as a local recreation area. The extensive park of the former St. Raphael Monastery north of the Lousberg was integrated into the Lousberg Park in 2009. The Lousberg is also the site of the annual summer Lousberg Run and the open-air literature festival &quot;Reading Pleasure on the Lousberg&quot;.

Geographic entities mentioned:
surface_form: lousberg
instance_of: Mountain
countries: Germany
coordinates: lat: 50.7869
lon: 6.07917
surface_form: lousberg
instance_of: Mountain
countries: Germany
coordinates: lat: 50.7869
lon: 6.07917
Today, the Lousberg is largely wooded and serves as a local recreation area. The extensive park of the former St. Raphael Monastery north of the Lousberg was integrated into the Lousberg Park in 2009. The Lousberg is also the site of the annual summer Lousberg Run and the open-air literature festival &quot;Reading Pleasure on the Lousberg&quot;. Legend.

Geographic entities mentioned:
surface_form: lousberg
instance_of: Mountain
countries: Germany
coordinates: lat: 50.7869
lon: 6.07917
Another explanation has to do with the Aachen dialect term &quot;lous&quot;, which means &quot;clever&quot;. Geology, formation. Geologically, the Lousberg is one of Aachen's three inlier mountains, along with the and the, and one of the southernmost foothills of the Aachen-Limburg Cretaceous.

Geographic entities mentioned:
surface_form: limburg
instance_of: Mountain
countries: Germany
coordinates: lat: 48.6042
lon: 9.53639
Kelleys Island, Ohio. Kelleys Island is both a village in Erie County, Ohio, and the island which it fully occupies in Lake Erie. The island has a total area of and was formed by glacial action on limestone and dolomite. As of the 2020 census it has a year-round population of under 300 and is primarily a vacation destination with a large seasonal influx of visitors and workers. History.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
state of Montana. It is situated one mile east of the Continental Divide, in Glacier County. It can be seen from the Many Glacier area, and up close from the Grinnell Glacier Trail. Topographic relief is significant as the north aspect rises nearly above Grinnell Lake in one-half mile. Climate.

Geographic entities mentioned:
surface_form: Grinnell Lake
instance_of: Lake
countries: United States
coordinates: lat: 48.766111111111
lon: -113.70416666667
Angel Wing (Glacier National Park). Angel Wing is a elevation mountain summit located in the Lewis Range, of Glacier National Park in the U.S. state of Montana. It is situated one mile east of the Continental Divide, in Glacier County. It can be seen from the Many Glacier area, and up close from the Grinnell Glacier Trail.

Geographic entities mentioned:
surface_form: angel wing
instance_of: Mountain
countries: United States
coordinates: lat: 48.7573144
lon: -113.7117691
Topographic relief is significant as the north aspect rises nearly above Grinnell Lake in one-half mile. Climate. Based on the Köppen climate classification, Angel Wing is located in an alpine subarctic climate zone with long, cold, snowy winters, and cool to warm summers. Temperatures can drop below −10 °F with wind chill factors below −30 °F.

Geographic entities mentioned:
surface_form: angel wing
instance_of: Mountain
countries: United States
coordinates: lat: 48.7573144
lon: -113.7117691
Geology. Like other mountains in Glacier National Park, Angel Wing is composed of sedimentary rock laid down during the Precambrian to Jurassic periods. Formed in shallow seas, this sedimentary rock was initially uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of precambrian rocks thick, wide and long over younger rock of the cretaceous period.

Geographic entities mentioned:
surface_form: angel wing
instance_of: Mountain
countries: United States
coordinates: lat: 48.7573144
lon: -113.7117691
Lake Firlej is a lake in east Poland in Lubartów County near the village of Firlej. The lake has no tributaries and no permanent outlets. The periodic flow only exists after thaws or heavy rains. It flows from its western side and into the lower Kunów Lake. Around the lake there is an illuminated footpath for pedestrians and a bicycle path. In summer, Lake Firlej is a popular vacation spot.

Geographic entities mentioned:
surface_form: Kunów Lake
instance_of: Lake
countries: Poland
coordinates: lat: 51.55
lon: 22.5
Lake Firlej. Lake Firlej is a lake in east Poland in Lubartów County near the village of Firlej. The lake has no tributaries and no permanent outlets. The periodic flow only exists after thaws or heavy rains. It flows from its western side and into the lower Kunów Lake. Around the lake there is an illuminated footpath for pedestrians and a bicycle path.

Geographic entities mentioned:
surface_form: lake firlej
instance_of: Lake
countries: Poland
coordinates: lat: 51.553611111111
lon: 22.516388888889
surface_form: firlej
instance_of: Lake
countries: Poland
coordinates: lat: 51.553611111111
lon: 22.516388888889
Lake Firlej. Lake Firlej is a lake in east Poland in Lubartów County near the village of Firlej. The lake has no tributaries and no permanent outlets. The periodic flow only exists after thaws or heavy rains. It flows from its western side and into the lower Kunów Lake. Around the lake there is an illuminated footpath for pedestrians and a bicycle path.

Geographic entities mentioned:
surface_form: lake firlej
instance_of: Lake
countries: Poland
coordinates: lat: 51.553611111111
lon: 22.516388888889
surface_form: firlej
instance_of: Lake
countries: Poland
coordinates: lat: 51.553611111111
lon: 22.516388888889
surface_form: firlej
instance_of: Lake
countries: Poland
coordinates: lat: 51.553611111111
lon: 22.516388888889
The periodic flow only exists after thaws or heavy rains. It flows from its western side and into the lower Kunów Lake. Around the lake there is an illuminated footpath for pedestrians and a bicycle path. In summer, Lake Firlej is a popular vacation spot. Several sandy beaches are scattered around the lake, Beach on Lake Firlej (Plaża nad jeziorem Firlej) being the largest.

Geographic entities mentioned:
surface_form: lake firlej
instance_of: Lake
countries: Poland
coordinates: lat: 51.553611111111
lon: 22.516388888889
surface_form: firlej
instance_of: Lake
countries: Poland
coordinates: lat: 51.553611111111
lon: 22.516388888889
Around the lake there is an illuminated footpath for pedestrians and a bicycle path. In summer, Lake Firlej is a popular vacation spot. Several sandy beaches are scattered around the lake, Beach on Lake Firlej (Plaża nad jeziorem Firlej) being the largest. The area around the lake is forested to the south, and more populated on the north side.

Geographic entities mentioned:
surface_form: lake firlej
instance_of: Lake
countries: Poland
coordinates: lat: 51.553611111111
lon: 22.516388888889
surface_form: firlej
instance_of: Lake
countries: Poland
coordinates: lat: 51.553611111111
lon: 22.516388888889
surface_form: firlej
instance_of: Lake
countries: Poland
coordinates: lat: 51.553611111111
lon: 22.516388888889
The area around the lake is forested to the south, and more populated on the north side. The village of Firlej is situated on the north-west side of the lake. Fishing from piers and boats is possible on Lake Firlej. Many species of fish live in the lake, including bream, roach, pike, zander, crucian carp, and eel.

Geographic entities mentioned:
surface_form: lake firlej
instance_of: Lake
countries: Poland
coordinates: lat: 51.553611111111
lon: 22.516388888889
surface_form: firlej
instance_of: Lake
countries: Poland
coordinates: lat: 51.553611111111
lon: 22.516388888889
In summer, Lake Firlej is a popular vacation spot. Several sandy beaches are scattered around the lake, Beach on Lake Firlej (Plaża nad jeziorem Firlej) being the largest. The area around the lake is forested to the south, and more populated on the north side. The village of Firlej is situated on the north-west side of the lake. Fishing from piers and boats is possible on Lake Firlej.

Geographic entities mentioned:
surface_form: firlej
instance_of: Lake
countries: Poland
coordinates: lat: 51.553611111111
lon: 22.516388888889
Census Bureau, the county has a total area of, of which is land and (0.4%) is water. The county is located in the Blue Ridge Mountains. The summit of Blood Mountain, which Lumpkin County shares with Union County to the north, is the highest point in the county. At, Blood Mountain is the fifth-highest peak in Georgia and the highest point on Georgia's portion of the Appalachian Trail.

Geographic entities mentioned:
surface_form: Blood Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 34.73972222222222
lon: -83.9375
The western 40% of Lumpkin County is located in the Etowah River sub-basin of the ACT River Basin (Alabama-Coosa-Tallapoosa River Basin), while the eastern 60% of the county is located in the Upper Chattahoochee River sub-basin of the ACF River Basin (Apalachicola-Chattahoochee-Flint River Basin). Penitentiary Cove is located in the north/northwest part of Lumpkin County. Demographics.

Geographic entities mentioned:
surface_form: Chattahoochee River
instance_of: Watercourse
countries: United States
coordinates: lat: 30.7088028
lon: -84.8638097
The western 40% of Lumpkin County is located in the Etowah River sub-basin of the ACT River Basin (Alabama-Coosa-Tallapoosa River Basin), while the eastern 60% of the county is located in the Upper Chattahoochee River sub-basin of the ACF River Basin (Apalachicola-Chattahoochee-Flint River Basin). Penitentiary Cove is located in the north/northwest part of Lumpkin County. Demographics.

Geographic entities mentioned:
surface_form: Penitentiary Cove
instance_of: Valley
countries: United States
coordinates: lat: 34.62898
lon: -84.13686
While many of them crumbled with time, a few survived the ravages of nature - as for example, the temples at Pakbirra, Deulghata, Deulia and Banda
Area overview. Purulia district forms the lowest step of the Chota Nagpur Plateau. The general scenario is undulating land with scattered hills. Purulia Sadar subdivision covers the central portion of the district.

Geographic entities mentioned:
surface_form: Chota Nagpur Plateau
instance_of: Plateau
countries: India
coordinates: lat: 23
lon: 85
Warren Landing Lower Range Lights. The Warren Landing Lower Range Lights are a pair of range lights in Warren Landing, Manitoba, at the entrance to the Nelson River. Built in 1908, the lighthouses help to guide ship traffic from Lake Winnipeg into the river. They work in tandem with the Warren Landing Upper Range Lights.

Geographic entities mentioned:
surface_form: Lake Winnipeg
instance_of: Lake
countries: Canada
coordinates: lat: 52.116666666667
lon: -97.25
Mount Pinatubo Eruption. When the population was put into a state of alert during the first phases of the Pinatubo crisis, authorities from the NDCC showed indisputable efficiency in managing the people. Precautionary Measures Before Sensing an Eruption. Prior the eruption, no precautionary measures were taken until signs of activity were observed in 1991.

Geographic entities mentioned:
surface_form: Pinatubo
instance_of: Mountain
countries: Philippines
coordinates: lat: 15.13
lon: 120.35
On the day of June 26, 1991, orders of evacuation were conveyed to local authorities or Coordination Councils (DCC). During those times, the entire zone located within the 10 km radius around the crater of Pinatubo has been decreed as permanent high risk sector by PHIVOLCS prohibiting all human occupation of the zone.

Geographic entities mentioned:
surface_form: Pinatubo
instance_of: Mountain
countries: Philippines
coordinates: lat: 15.13
lon: 120.35
In the time of Pinatubo’s eruptive phase in June 1991, most of the population reacted favorably to the evacuation orders due to the early preparation and coordination efforts the authorities on the field have demonstrated. However, there were still some Aetas that changed their minds and decided to return to the mountains seeking refuge in caves and spiritual comfort from their God.

Geographic entities mentioned:
surface_form: Pinatubo
instance_of: Mountain
countries: Philippines
coordinates: lat: 15.13
lon: 120.35
Old County Gaol (Jail). Originally built in 1840 and located in Kingston, the granite blocks of the jail were dismantled and hauled piece by piece from Kingston to Hampton by oxen and horses over road and the ice of the Kennebecasis River in 1871, when Hampton became the new shire-town of Kings County. It was then rebuilt where it now stands and remained in use as a jail until 1971.

Geographic entities mentioned:
surface_form: Kennebecasis River
instance_of: Watercourse
countries: Canada
coordinates: lat: 45.31666667
lon: -66.13333333
Course. It forms on Cobb Mountain at above sea level and drops to at Clear Lake. It flows in a northwest direction through the mountains to Big Valley, then flows north to the lake, which it enters through Clear Lake State Park. At its mouth it is called Kelsey Slough. Kelseyville is the largest community in the watershed, on the east side of Big Valley.

Geographic entities mentioned:
surface_form: Cobb Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.8074
lon: -122.741
It is about 10% of the Clear Lake watershed, and contributes about 16% of the water flowing into the lake. The highest point is the summit of Cobb Mountain at above sea level, and the lowest area is the flat farmlands of Big Valley beside Clear Lake at above sea level. Geothermal field.

Geographic entities mentioned:
surface_form: Cobb Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.8074
lon: -122.741
Most of this came from the volcanic uplands of Kelsey Creek and neighboring watersheds. By the end of the 19th century most of the prime timber in the Boggs Mountain area had been cleared, and the land was mainly being used for pasturage rather than timber. After World War II (1939–1945) there was a boom in construction, and all the usable old-growth and secondary forest was clear cut.

Geographic entities mentioned:
surface_form: Boggs Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.815555555556
lon: -122.68277777778
Road improvements in the 1910s and 1920s resulted in new resorts being opened along the roads. In the early 1920s, Jim McCauley established a resort on the creek between Cobb and Whispering Pines, west of his Boggs Mountain property. It was originally named Camp Calso but renamed to Forest Lake Resort in 1938. McCauley dammed a tributary of Kelsey Creek to create Lake McCauley in 1935.

Geographic entities mentioned:
surface_form: Boggs Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.815555555556
lon: -122.68277777778
The effects are also spilling over into Marina del Rey and Hermosa Beach. Start-up pockets have also emerged in nearby Culver City, West L.A., and El Segundo. Other pockets include Downtown Los Angeles, Beverly Hills, Hollywood, Glendale, and the San Fernando Valley.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
Mount Avalanche. Mount Avalanche is a mountain in New Zealand. Description. Mount Avalanche is located four kilometres south of Tititea in the Southern Alps. The summit is set on the boundary shared by the Otago and West Coast Regions of the South Island. It is also within Mount Aspiring National Park which is part of the Te Wahipounamu UNESCO World Heritage Site.

Geographic entities mentioned:
surface_form: Tititea
instance_of: Mountain
countries: New Zealand
coordinates: lat: -44.384
lon: 168.728
surface_form: mount avalanche
instance_of: Mountain
countries: New Zealand
coordinates: lat: -44.422
lon: 168.741
Mount Avalanche. Mount Avalanche is a mountain in New Zealand. Description. Mount Avalanche is located four kilometres south of Tititea in the Southern Alps. The summit is set on the boundary shared by the Otago and West Coast Regions of the South Island. It is also within Mount Aspiring National Park which is part of the Te Wahipounamu UNESCO World Heritage Site.

Geographic entities mentioned:
surface_form: mount avalanche
instance_of: Mountain
countries: New Zealand
coordinates: lat: -44.422
lon: 168.741
Climate. Based on the Köppen climate classification, Mount Avalanche is located in a marine west coast climate zone, with a subpolar oceanic climate (Cfc) at the summit. Prevailing westerly winds blow moist air from the Tasman Sea onto the mountain, where the air is forced upwards by the mountains (orographic lift), causing moisture to drop in the form of rain and snow.

Geographic entities mentioned:
surface_form: mount avalanche
instance_of: Mountain
countries: New Zealand
coordinates: lat: -44.422
lon: 168.741
According to the &quot;District Census Handbook 2011, Puruliya&quot;, Jhalda municipality covered an area of. Area overview. Purulia district forms the lowest step of the Chota Nagpur Plateau. The general scenario is undulating land with scattered hills. Jhalda subdivision, shown in the map alongside, is located in the western part of the district, bordering Jharkhand.

Geographic entities mentioned:
surface_form: Chota Nagpur Plateau
instance_of: Plateau
countries: India
coordinates: lat: 23
lon: 85
Loch Bhac. Loch Bhac (Bhaic or Vach) is a fine freshwater trout loch, located in the west part of the Allean Forest, and east part of Tay Forest park, and slightly north of Loch Tummel, within Perth and Kinross, Scotland. Loch Bhac sits on a south-west to north-east orientation.

Geographic entities mentioned:
surface_form: loch bhac
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.733333333333
lon: -3.9166666666667
Savalen. Savalen is a lake in Innlandet country, Norway. The lake is located along the border of Tynset Municipality and Alvdal Municipality. The lake sits about west of the town of Tynset and about north of the village of Alvdal. The river Sivilla, which connects the lake Savalen and the large river Glomma, is regulated and exploited by the Savalen hydropower station.

Geographic entities mentioned:
surface_form: savalen
instance_of: Lake
countries: Norway
coordinates: lat: 62.241111111111
lon: 10.482222222222
The lake sits about west of the town of Tynset and about north of the village of Alvdal. The river Sivilla, which connects the lake Savalen and the large river Glomma, is regulated and exploited by the Savalen hydropower station. A tourist resort is located at the northern end of the lake, with facilities for winter sports. The skating stadium is the highest elevation skating venue in Norway.

Geographic entities mentioned:
surface_form: savalen
instance_of: Lake
countries: Norway
coordinates: lat: 62.241111111111
lon: 10.482222222222
surface_form: savalen
instance_of: Lake
countries: Norway
coordinates: lat: 62.241111111111
lon: 10.482222222222
Notable seaside beaches can be found at Marin Headlands and Point Reyes National Seashore in the south, with innumerable examples of remote or less used beaches north of the San Francisco Bay area.

Geographic entities mentioned:
surface_form: Marin Headlands
instance_of: Landform
countries: United States
coordinates: lat: 37.827777777778
lon: -122.50611111111
Maddock was a Creative Arts Fellow at the Australian National University, Canberra in 1976. Maddock lived and worked at Mount Macedon, Victoria until the Ash Wednesday fires of 1983 forced her to flee. Her house, studio and a large archive of many decades' work were destroyed. She later returned to her native state of Tasmania.

Geographic entities mentioned:
surface_form: Mount Macedon
instance_of: Mountain
countries: Australia
coordinates: lat: -37.38291
lon: 144.57625
Kralingse Plas. The Kralingse Plas is a lake located in the suburb of Kralingen in Rotterdam, the Netherlands. The water is mainly used for watersport, fishing and recreational activities. The Kralingse Plas was created due to peat extractions.

Geographic entities mentioned:
surface_form: kralingse plas
instance_of: Lake
countries: Netherlands
coordinates: lat: 51.934722
lon: 4.515
The fighting died down and the new line was held through the summer months. CCLXVI Brigade moved down to the Jordan Valley with 158th Infantry Bde in late March to cover the EEF's First Transjordan raid, then rejoined the rest of the division at Ramallah at the beginning of April.

Geographic entities mentioned:
surface_form: Jordan Valley
instance_of: Valley
countries: Jordan
coordinates: lat: 32.317222
lon: 35.57
Goch fell on 21 February. 53rd Division was not involved in the assault crossing of the Rhine (Operation Plunder) on 23/24 March, but it crossed on 26 March and the next day attacked through Hamminkeln to Dingden. It then took part in the drive to the Elbe. The German surrender at Lüneburg Heath, ending the fighting on 21st Army Group's front, came on 4 May.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
Wolbrom. Wolbrom (,) is a town in Olkusz County, Lesser Poland Voivodeship, in southern Poland, with 8,942 people (2010). Wolbrom lies in the Kraków-Częstochowa Upland, which is also called the &quot;Polish Jura&quot;. South of the town there is &quot;Kamienna Mountain&quot;, with a steel cross on top, and a great view of Wolbrom. The town lies above sea level, and its area, was.

Geographic entities mentioned:
surface_form: Kraków-Częstochowa Upland
instance_of: Plateau
countries: Poland
coordinates: lat: 50.2067
lon: 19.8292
Wonalancet River. The Wonalancet River is a river in the White Mountains of New Hampshire in the United States. Named after the 17th-century Pennacook sachem Wonalancet, it is a tributary of the southern Swift River, part of the Bearcamp River / Ossipee Lake / Saco River watershed leading to the Atlantic Ocean.

Geographic entities mentioned:
surface_form: Ossipee Lake
instance_of: Lake
countries: United States
coordinates: lat: 43.791388888889
lon: -71.139722222222
The Wonalancet River rises in the heart of the Sandwich Range, in &quot;The Bowl&quot;, a forested glacial cirque lying between Mount Whiteface to the west, Mount Passaconaway to the north, and Mount Wonalancet to the east.

Geographic entities mentioned:
surface_form: Mount Whiteface
instance_of: Mountain
countries: United States
coordinates: lat: 43.933961111111
lon: -71.405905555556
surface_form: Mount Passaconaway
instance_of: Mountain
countries: United States
coordinates: lat: 43.954722222222
lon: -71.381388888889
surface_form: Mount Wonalancet
instance_of: Mountain
countries: United States
coordinates: lat: 43.926666666667
lon: -71.376666666667
Lake Vrana (Cres). Lake Vrana (), in the centre of Cres island, is a fresh water lake, wide and about long. The town of Cres has been supplied with drinking water from the lake since 1953, and the towns of Mali and Veli Lošinj received their supplies ten years later.

Geographic entities mentioned:
surface_form: vrana
instance_of: Lake
countries: Croatia
coordinates: lat: 44.8549
lon: 14.3852
surface_form: lake vrana
instance_of: Lake
countries: Croatia
coordinates: lat: 44.8549
lon: 14.3852
surface_form: lake vrana
instance_of: Lake
countries: Croatia
coordinates: lat: 43.89
lon: 15.57
Comprising an area of, the depression reaches a depth of around below the sea level, but its surface lies about above it, oscillating by about half a metre, meaning the maximum depth is. It is surrounded by mountains like the high Mount Elmo and Mount Perskra of. The village of Vrana, above the lake, is located south of the town of Cres. The lake contains pike, tench and carp.

Geographic entities mentioned:
surface_form: vrana
instance_of: Lake
countries: Croatia
coordinates: lat: 44.8549
lon: 14.3852