Sarmila/GeoWiki-Features huggingface dataset:
The population grew by 1.6% (522 persons) between the 1992 and 2002 censuses. The main settlements of the commune are the city of Victoria and the villages of Selva Oscura, Púa and Quino. Attractions. Some snowcapped volcanoes of the Andes, such as the Tolhuaca, Lonquimay, Sierra Nevada and the Llaima, can be seen from Victoria, forming an enormous backdrop for the city. Economy.

Geographic entities mentioned:
surface_form: Llaima
instance_of: Mountain
countries: Chile
coordinates: lat: -38.697407
lon: -71.730445
Its privileged location in the center of the Province, close to the regional capital, Temuco, permits an expedite connection with the main national routes such as railways and Chile Route 5. It is also located halfway along the bi-oceanic corridor between the Pacific Ocean and Argentina across the Pino Hachado Pass. Administration.

Geographic entities mentioned:
surface_form: Pino Hachado Pass
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -38.65
lon: -70.88333333
Watershed and course. Arroyo Bayo arises at then flows west-northwest along Mount Hamilton Road then turns north where it is joined by San Antonio Creek to form Arroyo Valle. Arroyo Valle flows north through Lake Del Valle to the Livermore Valley where it turns west to Arroyo de la Laguna at Interstate 680, ultimately joining Alameda Creek and terminating in San Francisco Bay. Habitat and Ecology.

Geographic entities mentioned:
surface_form: Lake Del Valle
instance_of: Lake
countries: United States
coordinates: lat: 37.598333333333
lon: -121.72111111111
surface_form: Livermore Valley
instance_of: Valley
countries: United States
coordinates: lat: 37.6886
lon: -121.736
Lake Järvepää. Järvepää is a lake of Estonia.

Geographic entities mentioned:
surface_form: lake järvepää
instance_of: Lake
countries: Estonia
coordinates: lat: 57.95555556
lon: 27.47416667
Southern Great Lakes seismic zone. 3p63it68v6ueukexga1b9p34ms4g" xml:space="preserve">The Southern Great Lakes Seismic Zone is a zone of low to moderate seismic activity surrounding Lake Erie and Lake Ontario in Canada and the United States.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
Sarvant Glacier. The Sarvant Glacier is a glacier located on the northern slopes of the Cowlitz Chimneys in the state of Washington. Named for Henry M. Sarvant, who mapped Mount Rainier in 1894, the glacier starts at an elevation of about and descends northward down to. There are several patches of permanent ice and snow that lie to the east and west of the glacier.

Geographic entities mentioned:
surface_form: Cowlitz Chimneys
instance_of: Landform
countries: United States
coordinates: lat: 46.848877
lon: -121.609409
Pests of peach. See ' for the cause of here. Diseases of peach. UC IPM provides information about and. (See also.)
Peach Yellow Leaf Roll was first discovered in the Sacramento Valley in 1948, but remained uncommon until an epidemic in the late 1970s and early 1980s. For the causative organism see '. Integrated pest management in peach.

Geographic entities mentioned:
surface_form: Sacramento Valley
instance_of: Valley
countries: United States
coordinates: lat: 39
lon: -121.5
In August 1965, the &quot;Wall Street Journal&quot; reported that Wynne's development company, Great Southwest Corporation, had purchased of land along the Chattahoochee River outside of Atlanta for a planned $400 million industrial park with an adjacent $7 million amusement park.

Geographic entities mentioned:
surface_form: Chattahoochee River
instance_of: Watercourse
countries: United States
coordinates: lat: 30.7088028
lon: -84.8638097
has been the scene of two fatal incidents nearly identical in nature, where individuals were underneath the attraction while it was operational and were struck and killed by the train itself or by the riders' exposed legs. Portions of Six Flags Over Georgia lie within the flood plain of the Chattahoochee River, which has caused occasional problems whenever the river overflows its banks.

Geographic entities mentioned:
surface_form: Chattahoochee River
instance_of: Watercourse
countries: United States
coordinates: lat: 30.7088028
lon: -84.8638097
Hohenstoffeln. Hohenstoffeln is a double peaked mountain of volcanic origin in the Hegau region (Konstanz district) of southern Baden-Württemberg, Germany.

Geographic entities mentioned:
surface_form: Hegau
instance_of: Mountain
countries: Germany
coordinates: lat: 47.795
lon: 8.75
surface_form: hohenstoffeln
instance_of: Mountain
countries: Germany
coordinates: lat: 47.796388888889
lon: 8.7497222222222
Hohenstoffeln. Hohenstoffeln is a double peaked mountain of volcanic origin in the Hegau region (Konstanz district) of southern Baden-Württemberg, Germany.

Geographic entities mentioned:
surface_form: hohenstoffeln
instance_of: Mountain
countries: Germany
coordinates: lat: 47.796388888889
lon: 8.7497222222222
Thietgaud was now freed from the ban, but Gunther remained excommunicated until the summer of 869, when, after a public retraction (P. L., CXXI, 381), he was admitted by the pope to lay communion at Monte Cassino abbey. The See of Cologne had in 864 been given by Lothair to the subdeacon Hugh, a nephew of Charles the Bald. He was deposed in 866 and Gunther regained his see.

Geographic entities mentioned:
surface_form: Monte Cassino
instance_of: Mountain
countries: Italy
coordinates: lat: 41.49
lon: 13.813888888889
Mapped by the USGS from tellurometer surveys and Navy air photos, 1960-62. Named by US-ACAN for Ellsworth C. Dougherty, USARP biologist at McMurdo Sound, 1959-60 and 1961-62. Mount Cara. Peak, high, standing north-northwest of Mount Lysaght. Named by the British Antarctic Expedition, 1907–09.

Geographic entities mentioned:
surface_form: Mount Lysaght
instance_of: Mountain
coordinates: lat: -82.8167
lon: 161.317
Svaton Peaks. Svaton Peaks () is a cluster of rugged peaks at the north end of the Queen Elizabeth Range, Antarctica, surmounting the area between the mouths of the Heilman Glacier and Otago Glacier. Exploration and name. The Svaton Peaks were mapped by the United States Geological Survey (USGS) from tellurometer surveys and Navy air photos, 1960–62.

Geographic entities mentioned:
surface_form: elizabeth
instance_of: Mountain
coordinates: lat: -83.9
lon: 168.383
surface_form: svaton peaks
instance_of: Mountain
coordinates: lat: -82.5833
lon: 161
Location. Svaton Peaks are in the north of the Queen Elizabeth Range at the north end of a block bounded by the Inaccessible Cliffs along the coast of the Nimrod Glacier to the north, the Hamilton Glacier to the west and the Otago Glacier to the east. Nearby features include the Heilman Glacier, Mount Hofmann, Mount Sandved, Mount Dougherty and Mount Cara. Inaccessible Cliffs.

Geographic entities mentioned:
surface_form: elizabeth
instance_of: Mountain
coordinates: lat: -83.9
lon: 168.383
surface_form: svaton peaks
instance_of: Mountain
coordinates: lat: -82.5833
lon: 161
Nearby features include the Heilman Glacier, Mount Hofmann, Mount Sandved, Mount Dougherty and Mount Cara. Inaccessible Cliffs. A line of steep cliffs, interrupted by several glaciers, which form the northern escarpment of the Queen Elizabeth Range. The escarpment borders the southern side of the Nimrod Glacier which is very heavily crevassed.

Geographic entities mentioned:
surface_form: elizabeth
instance_of: Mountain
coordinates: lat: -83.9
lon: 168.383
Mapped by the USGS from tellurometer surveys and Navy air photos, 1960-62. Named by US-ACAN for Walther F. Hofmann, USARP glaciologist on the Ross Ice Shelf, 1962-63. Mount Sandved. Mountain, high, standing north of Mount Dougherty in the north part of the Queen Elizabeth Range. Mapped by the USGS from tellurometer surveys and Navy air photos, 1960-62. Named by US-ACAN for Kurt G.

Geographic entities mentioned:
surface_form: elizabeth
instance_of: Mountain
coordinates: lat: -83.9
lon: 168.383
Named by US-ACAN for Kurt G. Sandved, Information Officer at the Office of Antarctic Programs, National Science Foundation. Mount Dougherty. A mountain, high, between Mount Sandved and Mount Cara on the main north–south ridge in the north part of the Queen Elizabeth Range. Mapped by the USGS from tellurometer surveys and Navy air photos, 1960-62. Named by US-ACAN for Ellsworth C.

Geographic entities mentioned:
surface_form: elizabeth
instance_of: Mountain
coordinates: lat: -83.9
lon: 168.383
Inaccessible Cliffs. A line of steep cliffs, interrupted by several glaciers, which form the northern escarpment of the Queen Elizabeth Range. The escarpment borders the southern side of the Nimrod Glacier which is very heavily crevassed. Named by the northern party of the NZGSAE (1961-62) because of their general inaccessibility. Mount Hofmann.

Geographic entities mentioned:
surface_form: southern
instance_of: Mountain
coordinates: lat: -74.2
lon: -76.4667
Location. Svaton Peaks are in the north of the Queen Elizabeth Range at the north end of a block bounded by the Inaccessible Cliffs along the coast of the Nimrod Glacier to the north, the Hamilton Glacier to the west and the Otago Glacier to the east. Nearby features include the Heilman Glacier, Mount Hofmann, Mount Sandved, Mount Dougherty and Mount Cara. Inaccessible Cliffs.

Geographic entities mentioned:
surface_form: hofmann
instance_of: Mountain
coordinates: lat: -82.6667
lon: 160.6
surface_form: mount hofmann
instance_of: Mountain
coordinates: lat: -82.6667
lon: 160.6
The escarpment borders the southern side of the Nimrod Glacier which is very heavily crevassed. Named by the northern party of the NZGSAE (1961-62) because of their general inaccessibility. Mount Hofmann. Snow-covered mountain, high, between the mouths of Hamilton Glacier and Heilman Glacier. Mapped by the USGS from tellurometer surveys and Navy air photos, 1960-62. Named by US-ACAN for Walther F.

Geographic entities mentioned:
surface_form: hofmann
instance_of: Mountain
coordinates: lat: -82.6667
lon: 160.6
surface_form: mount hofmann
instance_of: Mountain
coordinates: lat: -82.6667
lon: 160.6
Mount Hofmann. Snow-covered mountain, high, between the mouths of Hamilton Glacier and Heilman Glacier. Mapped by the USGS from tellurometer surveys and Navy air photos, 1960-62. Named by US-ACAN for Walther F. Hofmann, USARP glaciologist on the Ross Ice Shelf, 1962-63. Mount Sandved. Mountain, high, standing north of Mount Dougherty in the north part of the Queen Elizabeth Range.

Geographic entities mentioned:
surface_form: hofmann
instance_of: Mountain
coordinates: lat: -82.6667
lon: 160.6
Svaton Peaks. Svaton Peaks () is a cluster of rugged peaks at the north end of the Queen Elizabeth Range, Antarctica, surmounting the area between the mouths of the Heilman Glacier and Otago Glacier. Exploration and name. The Svaton Peaks were mapped by the United States Geological Survey (USGS) from tellurometer surveys and Navy air photos, 1960–62.

Geographic entities mentioned:
surface_form: svaton peaks
instance_of: Mountain
coordinates: lat: -82.5833
lon: 161
Exploration and name. The Svaton Peaks were mapped by the United States Geological Survey (USGS) from tellurometer surveys and Navy air photos, 1960–62. They were named by the United States Advisory Committee on Antarctic Names (US-ACAN) for Ernest M. Svaton, United States Antarctic Research Program (USARP) ionospheric physicist at McMurdo Station, winter 1963 and 1964. Location.

Geographic entities mentioned:
surface_form: svaton peaks
instance_of: Mountain
coordinates: lat: -82.5833
lon: 161
Golzerensee. __NOTOC__
Golzerensee (some times &quot;Golzernsee&quot;) is a lake at Golzeren (also &quot;Golzern&quot;) in the Canton of Uri, Switzerland. Its surface area is. Golzeren is located in the Maderanertal and can be reached by cable car from Bristen (municipality of Silenen). The lake is a popular fishing location. Species include brown trout, rainbow trout, and perch.

Geographic entities mentioned:
surface_form: Maderanertal
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.773333333333
lon: 8.7480555555556
surface_form: Bristen
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.7369
lon: 8.68135
surface_form: maderanertal
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.773333333333
lon: 8.7480555555556
surface_form: bristen
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.7369
lon: 8.68135
Golzerensee. __NOTOC__
Golzerensee (some times &quot;Golzernsee&quot;) is a lake at Golzeren (also &quot;Golzern&quot;) in the Canton of Uri, Switzerland. Its surface area is. Golzeren is located in the Maderanertal and can be reached by cable car from Bristen (municipality of Silenen). The lake is a popular fishing location. Species include brown trout, rainbow trout, and perch.

Geographic entities mentioned:
surface_form: golzernsee
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.775833333333
lon: 8.7397222222222
surface_form: golzerensee
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.775833333333
lon: 8.7397222222222
Golzerensee. __NOTOC__
Golzerensee (some times &quot;Golzernsee&quot;) is a lake at Golzeren (also &quot;Golzern&quot;) in the Canton of Uri, Switzerland. Its surface area is. Golzeren is located in the Maderanertal and can be reached by cable car from Bristen (municipality of Silenen). The lake is a popular fishing location. Species include brown trout, rainbow trout, and perch.

Geographic entities mentioned:
surface_form: golzerensee
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.775833333333
lon: 8.7397222222222
She is a Fellow of the Geological Society of America and the American Geophysical Union. Early life and education. Anderson was an undergraduate student in chemistry at the University of Puget Sound. The eruption of Mount St. Helens in May 1980 inspired her to study geosciences. At the University of Washington as a graduate student she was drawn to geomorphology and glaciology..

Geographic entities mentioned:
surface_form: Mount St. Helens
instance_of: Mountain
countries: United States
coordinates: lat: 46.200277777778
lon: -122.18944444444
Ai-Petri. Ai-Petri () is a peak in the Crimean Mountains. For administrative purposes it is in the Yalta municipality of Crimea. The name is of Greek origin, and translates as &quot;St. Peter&quot; (). Overview. Ai-Petri is one of the windiest places in Crimea. The wind blows for 125 days a year, reaching a speed of. The peak is located above the city of Alupka and the town of Koreiz.

Geographic entities mentioned:
surface_form: ai-petri
instance_of: Mountain
countries: Ukraine
Russia
Russian Empire
Soviet Union
coordinates: lat: 44.451111111111
lon: 34.052777777778
The wind blows for 125 days a year, reaching a speed of. The peak is located above the city of Alupka and the town of Koreiz. There is a cable car that takes passengers from a station near Alupka to the main area in Ai-Petri. The Ai-Petri massif makes up one side of the Grand Canyon of Crimea, with the other side being the. A military base is located here. It was attacked in May 2024.

Geographic entities mentioned:
surface_form: ai-petri
instance_of: Mountain
countries: Ukraine
Russia
Russian Empire
Soviet Union
coordinates: lat: 44.451111111111
lon: 34.052777777778
surface_form: ai-petri
instance_of: Mountain
countries: Ukraine
Russia
Russian Empire
Soviet Union
coordinates: lat: 44.451111111111
lon: 34.052777777778
The 51 mile (80k) Metacomet Trail traverses the range. Geography. Located within the towns of Meriden, Southington, and Berlin, the range, roughly horseshoe-shaped with cliff faces oriented south and west, includes, from east to west, Cathole Mountain, South Mountain, East Peak, and West Peak. Castle Craig is a small stone tower built in 1900 on East Peak.

Geographic entities mentioned:
surface_form: Cathole Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.5758
lon: -72.8006
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.182222222222
lon: -74.477777777778
surface_form: east peak
instance_of: Mountain
countries: United States
coordinates: lat: 38.9425
lon: -119.907
surface_form: east peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.912222222222
lon: -115.58277777778
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.949166666667
lon: -74.293333333333
surface_form: west peak
instance_of: Mountain
countries: United States
coordinates: lat: 47.7232516
lon: -123.3490055
surface_form: east peak
instance_of: Mountain
countries: United States
coordinates: lat: 41.5575
lon: -72.8372
surface_form: south mountain
instance_of: Landform
countries: United States
coordinates: lat: 40.33
lon: -76.2
surface_form: west peak
instance_of: Mountain
countries: United States
coordinates: lat: 41.5625
lon: -72.8444
surface_form: west peak
instance_of: Mountain
countries: United States
coordinates: lat: 46.779722222222
lon: -109.53638888889
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.5544
lon: -72.8236
surface_form: west peak
instance_of: Mountain
countries: United States
coordinates: lat: 45.73361111
lon: -112.48416667
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.40111111
lon: -109.26111111
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.189166666667
lon: -74.051666666667
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.361944444444
lon: -74.285277777778
surface_form: east peak
instance_of: Mountain
countries: United States
coordinates: lat: 61.15
lon: -146.045
Castle Craig is a small stone tower built in 1900 on East Peak. The Metacomet Ridge extends north from the Hanging Hills as Short Mountain and Ragged Mountain and southeast as Lamentation Mountain.

Geographic entities mentioned:
surface_form: Lamentation Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.574166666667
lon: -72.7625
surface_form: ragged mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.6175
lon: -72.8228
surface_form: short mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.7801
lon: -78.5408
surface_form: ragged mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.020277777778
lon: -110.75944444444
surface_form: hanging hills
instance_of: Mountain
countries: United States
coordinates: lat: 41.56
lon: -72.82
surface_form: short mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.0972
lon: -78.7428
surface_form: ragged mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.4681
lon: -71.8294
surface_form: short mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.6025
lon: -72.8242
Swimming is prohibited. Rock climbing is only permitted for Ragged Mountain Foundation members who have obtained a permit from Meriden's parks and recreation department. From the top of the Hanging Hills' many cliffs it is possible to see much of the Quinnipiac River Valley region, Long Island Sound, and the distant higher peaks of southern New England. Conservation.

Geographic entities mentioned:
surface_form: ragged mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.6175
lon: -72.8228
surface_form: ragged mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.020277777778
lon: -110.75944444444
surface_form: ragged mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.4681
lon: -71.8294
Several notable reservoirs and natural bodies of water are located within the Hanging Hills or beneath its slopes, including Kenmere Reservoir, Hallmere Reservoir, Elmere Reservoir, Beaver Pond, Silver Lake, Mirror Lake, and Slopers Ponds. Merimere Reservoir, nestled between South Mountain and East Peak and punctuated by the rocky mass of Mine Island, is considered particularly scenic. History.

Geographic entities mentioned:
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.182222222222
lon: -74.477777777778
surface_form: east peak
instance_of: Mountain
countries: United States
coordinates: lat: 38.9425
lon: -119.907
surface_form: east peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.912222222222
lon: -115.58277777778
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.949166666667
lon: -74.293333333333
surface_form: east peak
instance_of: Mountain
countries: United States
coordinates: lat: 41.5575
lon: -72.8372
surface_form: south mountain
instance_of: Landform
countries: United States
coordinates: lat: 40.33
lon: -76.2
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.5544
lon: -72.8236
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.40111111
lon: -109.26111111
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.189166666667
lon: -74.051666666667
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.361944444444
lon: -74.285277777778
surface_form: east peak
instance_of: Mountain
countries: United States
coordinates: lat: 61.15
lon: -146.045
Several of these faults break the Metacomet Ridge north of Meriden. Stream erosion and glacial ice carved canyons along these faults, dividing the ridge into the finger-like promontories of the Hanging Hills. Merimere Reservoir was built in the fault-controlled valley between East Peak and South Mountain. Ecosystem. The Hanging Hills host a combination of microclimates unusual in New England.

Geographic entities mentioned:
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.182222222222
lon: -74.477777777778
surface_form: east peak
instance_of: Mountain
countries: United States
coordinates: lat: 38.9425
lon: -119.907
surface_form: east peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.912222222222
lon: -115.58277777778
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.949166666667
lon: -74.293333333333
surface_form: east peak
instance_of: Mountain
countries: United States
coordinates: lat: 41.5575
lon: -72.8372
surface_form: south mountain
instance_of: Landform
countries: United States
coordinates: lat: 40.33
lon: -76.2
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.5544
lon: -72.8236
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.40111111
lon: -109.26111111
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.189166666667
lon: -74.051666666667
surface_form: south mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.361944444444
lon: -74.285277777778
surface_form: east peak
instance_of: Mountain
countries: United States
coordinates: lat: 61.15
lon: -146.045
The 51 mile (80k) Metacomet Trail traverses the range. Geography. Located within the towns of Meriden, Southington, and Berlin, the range, roughly horseshoe-shaped with cliff faces oriented south and west, includes, from east to west, Cathole Mountain, South Mountain, East Peak, and West Peak. Castle Craig is a small stone tower built in 1900 on East Peak.

Geographic entities mentioned:
surface_form: east peak
instance_of: Mountain
countries: United States
coordinates: lat: 38.9425
lon: -119.907
surface_form: east peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.912222222222
lon: -115.58277777778
surface_form: east peak
instance_of: Mountain
countries: United States
coordinates: lat: 41.5575
lon: -72.8372
surface_form: east peak
instance_of: Mountain
countries: United States
coordinates: lat: 61.15
lon: -146.045
Basalt frequently breaks into octagonal and pentagonal columns, creating a unique &quot;postpile&quot; appearance. Huge slopes made of fractured basalt scree are visible beneath many of the ledges of the Hanging Hills; they are particularly visible along the base of East Peak where it plunges into Merimere Reservoir.

Geographic entities mentioned:
surface_form: east peak
instance_of: Mountain
countries: United States
coordinates: lat: 38.9425
lon: -119.907
surface_form: east peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.912222222222
lon: -115.58277777778
surface_form: hanging hills
instance_of: Mountain
countries: United States
coordinates: lat: 41.56
lon: -72.82
surface_form: east peak
instance_of: Mountain
countries: United States
coordinates: lat: 41.5575
lon: -72.8372
surface_form: east peak
instance_of: Mountain
countries: United States
coordinates: lat: 61.15
lon: -146.045
Hanging Hills. The Hanging Hills of south central Connecticut, United States, are a range of mountainous trap rock ridges overlooking the city of Meriden and the Quinnipiac River Valley below. They are a subrange of the narrow, linear Metacomet Ridge that extends from Long Island Sound near New Haven, Connecticut, north through the Connecticut River Valley of Massachusetts to the Vermont border.

Geographic entities mentioned:
surface_form: hanging hills
instance_of: Mountain
countries: United States
coordinates: lat: 41.56
lon: -72.82
Hanging Hills. The Hanging Hills of south central Connecticut, United States, are a range of mountainous trap rock ridges overlooking the city of Meriden and the Quinnipiac River Valley below. They are a subrange of the narrow, linear Metacomet Ridge that extends from Long Island Sound near New Haven, Connecticut, north through the Connecticut River Valley of Massachusetts to the Vermont border.

Geographic entities mentioned:
surface_form: hanging hills
instance_of: Mountain
countries: United States
coordinates: lat: 41.56
lon: -72.82
surface_form: river valley
instance_of: Valley
countries: United States
coordinates: lat: 35.36
lon: -93.37
A popular outdoor recreation resource, the range is known for its microclimate ecosystems, rare plant communities, and expansive views from cliffs that rise abruptly over above the surrounding landscape. The Hanging Hills encompass the Hubbard Park, designed with the help of landscape architect Frederick Law Olmsted. The 51 mile (80k) Metacomet Trail traverses the range. Geography.

Geographic entities mentioned:
surface_form: hanging hills
instance_of: Mountain
countries: United States
coordinates: lat: 41.56
lon: -72.82
The Metacomet Ridge extends north from the Hanging Hills as Short Mountain and Ragged Mountain and southeast as Lamentation Mountain. The south, east, and west sides of the Hanging Hills drain into the Quinnipiac River, thence into Long Island Sound; the north side into the Mattabesset River, to the Connecticut River, thence to Long Island Sound.

Geographic entities mentioned:
surface_form: hanging hills
instance_of: Mountain
countries: United States
coordinates: lat: 41.56
lon: -72.82
surface_form: long island
instance_of: Landform
countries: United States
coordinates: lat: 46.7269
lon: -90.785
surface_form: long island
instance_of: Landform
countries: United States
coordinates: lat: 46.7269
lon: -90.785
History. The Hanging Hills' Hubbard Park was financed by Walter Hubbard, local entrepreneur and president of the Bradley & Hubbard Manufacturing Company. Hubbard elicited the assistance of eminent landscape architect Frederick Law Olmsted in drawing up the design.

Geographic entities mentioned:
surface_form: hanging hills
instance_of: Mountain
countries: United States
coordinates: lat: 41.56
lon: -72.82
Geology. The fault-block Hanging Hills were formed 200 million years ago during the Triassic and Jurassic periods and are composed of trap rock, also known as basalt, an extrusive volcanic rock. Basalt is a dark colored rock, but the iron within it weathers to a rusty brown when exposed to the air, lending the ledges a distinct reddish appearance.

Geographic entities mentioned:
surface_form: hanging hills
instance_of: Mountain
countries: United States
coordinates: lat: 41.56
lon: -72.82
Several of these faults break the Metacomet Ridge north of Meriden. Stream erosion and glacial ice carved canyons along these faults, dividing the ridge into the finger-like promontories of the Hanging Hills. Merimere Reservoir was built in the fault-controlled valley between East Peak and South Mountain. Ecosystem. The Hanging Hills host a combination of microclimates unusual in New England.

Geographic entities mentioned:
surface_form: hanging hills
instance_of: Mountain
countries: United States
coordinates: lat: 41.56
lon: -72.82
Talus slopes are especially rich in nutrients and support a number of calcium-loving plants uncommon in eastern Connecticut. Because the trap rock ridges generate such varied terrain, they are the home of several plant and animal species that are state-listed or globally rare. The Hanging Hills are also an important seasonal raptor migration path. Recreation.

Geographic entities mentioned:
surface_form: hanging hills
instance_of: Mountain
countries: United States
coordinates: lat: 41.56
lon: -72.82
Swimming is prohibited. Rock climbing is only permitted for Ragged Mountain Foundation members who have obtained a permit from Meriden's parks and recreation department. From the top of the Hanging Hills' many cliffs it is possible to see much of the Quinnipiac River Valley region, Long Island Sound, and the distant higher peaks of southern New England. Conservation.

Geographic entities mentioned:
surface_form: hanging hills
instance_of: Mountain
countries: United States
coordinates: lat: 41.56
lon: -72.82
surface_form: long island
instance_of: Landform
countries: United States
coordinates: lat: 46.7269
lon: -90.785
surface_form: river valley
instance_of: Valley
countries: United States
coordinates: lat: 35.36
lon: -93.37
A number of regional and local non-profit organizations are active in conserving the landscape and ecosystems of the Hanging Hills, most notably the Connecticut Forest and Park Association, the Meriden Land Trust, and the Berlin Land Trust.

Geographic entities mentioned:
surface_form: hanging hills
instance_of: Mountain
countries: United States
coordinates: lat: 41.56
lon: -72.82
Hubbard elicited the assistance of eminent landscape architect Frederick Law Olmsted in drawing up the design. Edwin Howard Armstrong, a network radio pioneer who invented FM radio, used West Peak as the location of one of the first FM radio broadcasts, in 1939. His original 70-foot (21 m) radio mast still stands on the peak.

Geographic entities mentioned:
surface_form: west peak
instance_of: Mountain
countries: United States
coordinates: lat: 47.7232516
lon: -123.3490055
surface_form: west peak
instance_of: Mountain
countries: United States
coordinates: lat: 41.5625
lon: -72.8444
surface_form: west peak
instance_of: Mountain
countries: United States
coordinates: lat: 46.779722222222
lon: -109.53638888889
surface_form: west peak
instance_of: Mountain
countries: United States
coordinates: lat: 45.73361111
lon: -112.48416667
Edwin Howard Armstrong, a network radio pioneer who invented FM radio, used West Peak as the location of one of the first FM radio broadcasts, in 1939. His original 70-foot (21 m) radio mast still stands on the peak. Currently, West Peak is home to seven FM broadcast stations, WPKT, WWYZ, WKSS, WDRC-FM, WZMX, WHCN and WMRQ-FM. Geology.

Geographic entities mentioned:
surface_form: west peak
instance_of: Mountain
countries: United States
coordinates: lat: 47.7232516
lon: -123.3490055
surface_form: west peak
instance_of: Mountain
countries: United States
coordinates: lat: 41.5625
lon: -72.8444
surface_form: west peak
instance_of: Mountain
countries: United States
coordinates: lat: 46.779722222222
lon: -109.53638888889
surface_form: west peak
instance_of: Mountain
countries: United States
coordinates: lat: 45.73361111
lon: -112.48416667
Eastern red cedar, a dry-loving species, clings to the barren edges of cliffs. Cooler north facing backslopes tend to support extensive stands of eastern hemlock interspersed with the oak-hickory forest species more common in the surrounding lowlands. Narrow ravines crowded with hemlock block sunlight, creating damp, cooler growing conditions with associated cooler climate plant species.

Geographic entities mentioned:
surface_form: hemlock
instance_of: Lake
countries: United States
coordinates: lat: 42.718611111111
lon: -77.608888888889
Hanging Hills. The Hanging Hills of south central Connecticut, United States, are a range of mountainous trap rock ridges overlooking the city of Meriden and the Quinnipiac River Valley below. They are a subrange of the narrow, linear Metacomet Ridge that extends from Long Island Sound near New Haven, Connecticut, north through the Connecticut River Valley of Massachusetts to the Vermont border.

Geographic entities mentioned:
surface_form: long island
instance_of: Landform
countries: United States
coordinates: lat: 46.7269
lon: -90.785
surface_form: river valley
instance_of: Valley
countries: United States
coordinates: lat: 35.36
lon: -93.37
Sierra Negra (Galápagos). Sierra Negra (Spanish: &quot;Black Mountain&quot;) is a large shield volcano at the southeastern end of Isabela Island in the Galapagos that rises to an altitude of 1124m. It coalesces with the volcanoes Cerro Azul to the west and Alcedo to the north.

Geographic entities mentioned:
surface_form: Alcedo
instance_of: Mountain
countries: Ecuador
coordinates: lat: -0.396583
lon: -91.109104
surface_form: cerro azul
instance_of: Mountain
countries: Ecuador
coordinates: lat: -0.91666666666667
lon: -91.408333333333
surface_form: azul
instance_of: Mountain
countries: Ecuador
coordinates: lat: -0.91666666666667
lon: -91.408333333333
surface_form: alcedo
instance_of: Mountain
countries: Ecuador
coordinates: lat: -0.396583
lon: -91.109104
Sierra Negra (Galápagos). Sierra Negra (Spanish: &quot;Black Mountain&quot;) is a large shield volcano at the southeastern end of Isabela Island in the Galapagos that rises to an altitude of 1124m. It coalesces with the volcanoes Cerro Azul to the west and Alcedo to the north.

Geographic entities mentioned:
surface_form: sierra negra (galápagos)
instance_of: Mountain
countries: Ecuador
coordinates: lat: -0.83
lon: -91.17
Sierra Negra (Galápagos). Sierra Negra (Spanish: &quot;Black Mountain&quot;) is a large shield volcano at the southeastern end of Isabela Island in the Galapagos that rises to an altitude of 1124m. It coalesces with the volcanoes Cerro Azul to the west and Alcedo to the north.

Geographic entities mentioned:
surface_form: sierra negra
instance_of: Mountain
countries: Ecuador
coordinates: lat: -0.83
lon: -91.17
Geology. The Sierra Negra like the other volcanoes on Isabela is believed to have been created from a mantle plume which has created the hotspot. The age of Sierra Negra and the other volcanoes on Isabela is hard to determine as they are in a north–south line to the east of the hotspot, which is believed to be under Fernandina volcano, and the Nazca Plate is moving east.

Geographic entities mentioned:
surface_form: sierra negra
instance_of: Mountain
countries: Ecuador
coordinates: lat: -0.83
lon: -91.17
This puts the volcanoes perpendicular to the hotspot. The surface of Sierra Negra and its neighbouring volcanoes are also covered by young lavas, adding to the difficulty of aging them. An estimate based on volume (588 km3) and eruption rates suggest that Sierra Negra is approximately 535,000 years old.

Geographic entities mentioned:
surface_form: sierra negra
instance_of: Mountain
countries: Ecuador
coordinates: lat: -0.83
lon: -91.17
An estimate based on volume (588 km3) and eruption rates suggest that Sierra Negra is approximately 535,000 years old. The morphology of Sierra Negra is the upturned soup bowl shape of the other Isabela volcanoes, however it does not have the steep sloping sides that are on others. Instead the slope goes from approximately 2 degrees at its base and although increasing averages only 5 degrees.

Geographic entities mentioned:
surface_form: sierra negra
instance_of: Mountain
countries: Ecuador
coordinates: lat: -0.83
lon: -91.17
The previous eruption began on 22 October 2005 and ended on 30 October 2005. That eruption was estimated to have produced 1.5x108 m3 of lava. Despite the GPS monitoring on Sierra Negra there was no advance warning of the eruption. There had been expansion of the caldera floor since 1992 but no short term deformational signal was noted before the eruption.

Geographic entities mentioned:
surface_form: sierra negra
instance_of: Mountain
countries: Ecuador
coordinates: lat: -0.83
lon: -91.17
Eradication efforts of feral goats were undertaken in Northern Isabela island, north of the Perry isthmus between Sierra Negra and Alcedo volcanoes but not in the southern portion of the island.

Geographic entities mentioned:
surface_form: sierra negra
instance_of: Mountain
countries: Ecuador
coordinates: lat: -0.83
lon: -91.17
surface_form: alcedo
instance_of: Mountain
countries: Ecuador
coordinates: lat: -0.396583
lon: -91.109104
The northern side of the volcano is almost entirely devoid of vegetation (with the exception of some cacti) as it has been resurfaced in more recent times by lava flows. The habitat for the Sierra Negra giant tortoise, &quot;Chelonoidis nigra guentheri&quot;, which has a saddleback shell, is on the southern and south eastern slopes of the volcano.

Geographic entities mentioned:
surface_form: sierra negra
instance_of: Mountain
countries: Ecuador
coordinates: lat: -0.83
lon: -91.17
It is composed of two villages, Colonia Târnava (&quot;Nagyekemezőtelep&quot;) and Târnava (formerly &quot;Proștea Mare&quot;). Geography. The commune is situated on the Transylvanian Plateau. It lies on the banks of the river Târnava Mare, in the northern part of the county, right in between the city of Mediaș and the town of Copșa Mică.

Geographic entities mentioned:
surface_form: Transylvanian Plateau
instance_of: Plateau
countries: Romania
coordinates: lat: 46.5
lon: 24.5
In January 1801, Martha freed his slaves. The Washington Monument was completed in 1885. Mount Rushmore, completed in 1941, has a gigantic Washington stone portrait sculpture to honor his presidency. In 2013, the Washington presidential library was completed and opened to the public. Background. George Washington, the first president elected under the U.S.

Geographic entities mentioned:
surface_form: Mount Rushmore
instance_of: Mountain
countries: United States
coordinates: lat: 43.878947222222
lon: -103.459825
In a profound symbolic sense, he &quot;was&quot; the new nation.&quot;
On December 6, 1884, the Washington Monument to honor George Washington was completed and was dedicated on February 21, 1885. In October 1941 the Mount Rushmore monument was completed that honored Washington first among three other presidents. Presidential library.

Geographic entities mentioned:
surface_form: Mount Rushmore
instance_of: Mountain
countries: United States
coordinates: lat: 43.878947222222
lon: -103.459825
With the privatization of the Japanese National Railways and the division of its assets, the Kyoto line came under the management of the West Japan Railway Company (JR West). The renaming of Saga Station to Saga-Urashima Station in 1994 was intended to associate it with the renowned district of Urashima, located in the western area of Kyoto Prefecture, thereby enhancing its tourism appeal.

Geographic entities mentioned:
surface_form: Urashima
instance_of: Mountain
countries: Japan
coordinates: lat: 35.00958333333333
lon: 135.6663888888889
Certain Easement Trails on AMR/AC lands are open to the public, with restrictions, and provide access to many of the High peaks trails: Basin Mountain, Mount Skylight, Mount Marcy, Mount Haystack, Mount Colvin, Nippletop Mountain, Dial Mountain, Lower Wolfjaw Mountain, Upper Wolfjaw Mountain, Armstrong Mountain, Gothics, Sawteeth, Saddleback Mountain, Noonmark Mountain, Round Mountain, and Rainbow and Beaver Meadow Falls.

Geographic entities mentioned:
surface_form: Mount Skylight
instance_of: Mountain
countries: United States
coordinates: lat: 44.0997
lon: -73.9308
surface_form: Mount Marcy
instance_of: Mountain
countries: United States
coordinates: lat: 44.112733333333
lon: -73.923727777778
surface_form: Mount Haystack
instance_of: Mountain
countries: United States
coordinates: lat: 44.1056
lon: -73.9006
surface_form: Mount Colvin
instance_of: Mountain
countries: United States
coordinates: lat: 44.0939
lon: -73.8344
surface_form: Dial Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.1059
lon: -73.796
surface_form: Lower Wolfjaw Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.1484
lon: -73.8326
surface_form: Upper Wolfjaw Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.1405
lon: -73.8453
surface_form: Gothics
instance_of: Mountain
countries: United States
coordinates: lat: 44.1281
lon: -73.8571
surface_form: Noonmark Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.1287
lon: -73.7726
Beede's was notorious for its austere accommodations, but no less famous for its setting near Upper and Lower Ausable Lakes and the Ausable River, and for its views of Giant and Noonmark Mountains, Sawteeth and Mount Colvin. Guides were available to lead parties up the rocky ravine of the Ausable to lean-to shelters on the lakes, and thence to the high peaks above.

Geographic entities mentioned:
surface_form: Giant
instance_of: Mountain
countries: United States
coordinates: lat: 44.1611
lon: -73.7202
They also reported that during the construction period, maintenance was also performed on a hydraulic elevator system in a tunnel under the statues. Description. Behind the central statues is a wall of the Korean Revolution Museum building, displaying a mosaic mural showing a scene from Mount Paektu, considered to be the sacred mountain of revolution.

Geographic entities mentioned:
surface_form: Mount Paektu
instance_of: Mountain
countries: North Korea
People's Republic of China
coordinates: lat: 41.992777777778
lon: 128.07722222222
Background. Following the First Mongol invasion of Hungary, King Béla IV ordered the construction of reinforced stone walls around the town of Buda and set his own royal palace on the top of the protecting hills of Buda, creating a new royal capital in the decades between 1247 and 1265. For defensive purposes, he moved the citizens of Pest to a hill on the opposite side of the Danube in 1248.

Geographic entities mentioned:
surface_form: a hill on the opposite side of the Danube
instance_of: Plateau
countries: Hungary
coordinates: lat: 47.5028
lon: 19.0317
The upper part of the river catchment area is also known as the Forth River High Country and contains the Cradle Mountain-Lake St Clair National Park, with the source of the river being on the southern slopes of Mount Pelion West. The catchment for the river is. There are several dams built on this river, including the Cethana, Devils Gate, and Paloona.

Geographic entities mentioned:
surface_form: Mount Pelion West
instance_of: Mountain
countries: Australia
coordinates: lat: -41.831677777778
lon: 145.977625
Anastas Ishirkov. Academic professor Anastas Todorov Ishirkov (; 5 April 1868 – 6 April 1937) was a Bulgarian scientist, geographer and ethnographer. He was the founder of geographical science in Bulgaria and was a member of Bulgarian Academy of Sciences. Honours. Ishirkov Crag on Oscar II Coast in Graham Land, Antarctica is named after Anastas Ishirkov.

Geographic entities mentioned:
surface_form: Ishirkov Crag
instance_of: Mountain
coordinates: lat: -65.39583333
lon: -62.5
In 1948 Massey was a crew member of the British boat which won the silver medal in the eights. Four years later he finished fourth with the British boat in the coxed fours competition. In 1949 and 1950, he was a member of the victorious Cambridge crew in the Boat Race. A mountain, Massey Heights, is named after him in Antarctica, and he was Master of the Worshipful Company of Grocers.

Geographic entities mentioned:
surface_form: Massey Heights
instance_of: Mountain
coordinates: lat: -63.9667
lon: -57.9667
Juniper Beach Provincial Park. Juniper Beach Provincial Park is a provincial park in the Thompson Country region of south central British Columbia, Canada. The facility is on the north side of the Thompson River, west of the town of Savona, and downstream from the Kamloops Lake outflow. On BC Highway 1, the locality is by road about east of Cache Creek and west of Kamloops. Facilities.

Geographic entities mentioned:
surface_form: Kamloops Lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.75
lon: -120.66666666666667
The city of Brookhaven, also in DeKalb County, joined in 2014. It is named for the Chattahoochee River, which forms the northern city limit of Sandy Springs and the southeastern city limit of Johns Creek. References. Public-private partnerships

Geographic entities mentioned:
surface_form: Chattahoochee River
instance_of: Watercourse
countries: United States
coordinates: lat: 30.7088028
lon: -84.8638097
Großer Sternberger See. Großer Sternberger See is a lake in Mecklenburg-Vorpommern, Germany. It has a surface area is 2.5 km² and is at an elevation of 8.6 m. It is located just east of the city of Sternberg.

Geographic entities mentioned:
surface_form: sternberger see
instance_of: Lake
countries: Germany
coordinates: lat: 53.716666666667
lon: 11.85
surface_form: großer sternberger see
instance_of: Lake
countries: Germany
coordinates: lat: 53.716666666667
lon: 11.85
Natives called it Namagonic (&quot;salmon trout spearing place&quot;). The lake is on a tributary of the Clyde River in Orleans County, Vermont. It is one of only two deep, cold, and oligotrophic lakes in the Clyde River system, the other being nearby Echo Lake. The closest major airport is located in Burlington, Vermont, located approximately 101 miles away. Dam.

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
Seymour Lake (Vermont). Seymour Lake is located in the town of Morgan in Orleans County, Vermont, United States, an area known as the Northeast Kingdom. The lake was named for Israel Seymour, one of the original grantees. Natives called it Namagonic (&quot;salmon trout spearing place&quot;). The lake is on a tributary of the Clyde River in Orleans County, Vermont.

Geographic entities mentioned:
surface_form: seymour lake
instance_of: Lake
countries: United States
coordinates: lat: 44.896
lon: -71.987
Historically the lake had a population of rainbow smelt, which was absent as of 2021. Environmental protection. The Aquatic Invasive Species Prevention Program of Seymour Lake was founded in 1999 for the protection against of Eurasian water milfoil (Myriophyllum spicatum) and zebra mussels (Dreissena polymorpha), which have already infested many nearby lakes but have not been found in Seymour.

Geographic entities mentioned:
surface_form: seymour lake
instance_of: Lake
countries: United States
coordinates: lat: 44.896
lon: -71.987