Sarmila/GeoWiki-Features huggingface dataset:
Castle Peak (Cowlitz County, Washington). Castle Peak is a mountain summit in Cowlitz County, Washington, United States. Description. Castle Peak ranks as the third-highest summit in Cowlitz County. It is located on the boundary shared by Mount St. Helens National Volcanic Monument and Gifford Pinchot National Forest.

Geographic entities mentioned:
surface_form: castle peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.3655
lon: -120.349
surface_form: castle peak
instance_of: Mountain
countries: United States
coordinates: lat: 61.597777777778
lon: -143.44361111111
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: castle peak
instance_of: Mountain
countries: United States
coordinates: lat: 44.0396
lon: -114.585
surface_form: castle peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.7731
lon: -106.834
surface_form: castle peak
instance_of: Mountain
countries: United States
coordinates: lat: 46.246388888889
lon: -122.2975
surface_form: castle peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.981944444444
lon: -120.86166666667
surface_form: castle peak
instance_of: Mountain
countries: United States
coordinates: lat: 32.3665
lon: -99.9995
surface_form: castle peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.0097
lon: -106.861
Castle Peak (Cowlitz County, Washington). Castle Peak is a mountain summit in Cowlitz County, Washington, United States. Description. Castle Peak ranks as the third-highest summit in Cowlitz County. It is located on the boundary shared by Mount St. Helens National Volcanic Monument and Gifford Pinchot National Forest.

Geographic entities mentioned:
surface_form: castle peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.3655
lon: -120.349
surface_form: castle peak
instance_of: Mountain
countries: United States
coordinates: lat: 61.597777777778
lon: -143.44361111111
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: castle peak
instance_of: Mountain
countries: United States
coordinates: lat: 44.0396
lon: -114.585
surface_form: castle peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.7731
lon: -106.834
surface_form: castle peak
instance_of: Mountain
countries: United States
coordinates: lat: 46.246388888889
lon: -122.2975
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: castle peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.981944444444
lon: -120.86166666667
surface_form: castle peak
instance_of: Mountain
countries: United States
coordinates: lat: 32.3665
lon: -99.9995
surface_form: castle peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.0097
lon: -106.861
Castle Peak (Cowlitz County, Washington). Castle Peak is a mountain summit in Cowlitz County, Washington, United States. Description. Castle Peak ranks as the third-highest summit in Cowlitz County. It is located on the boundary shared by Mount St. Helens National Volcanic Monument and Gifford Pinchot National Forest.

Geographic entities mentioned:
surface_form: castle peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.3655
lon: -120.349
surface_form: castle peak
instance_of: Mountain
countries: United States
coordinates: lat: 61.597777777778
lon: -143.44361111111
surface_form: castle peak
instance_of: Mountain
countries: United States
coordinates: lat: 44.0396
lon: -114.585
surface_form: castle peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.7731
lon: -106.834
surface_form: castle peak
instance_of: Mountain
countries: United States
coordinates: lat: 46.246388888889
lon: -122.2975
surface_form: castle peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.981944444444
lon: -120.86166666667
surface_form: castle peak
instance_of: Mountain
countries: United States
coordinates: lat: 32.3665
lon: -99.9995
surface_form: castle peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.0097
lon: -106.861
It is located on the boundary shared by Mount St. Helens National Volcanic Monument and Gifford Pinchot National Forest. Castle Peak is part of the Cascade Range, and it is situated west of Castle Lake. Topographic relief is significant as the summit rises above Castle Lake in one mile. Precipitation runoff from Castle Peak drains into tributaries of the South Fork and the North Fork Toutle River.

Geographic entities mentioned:
surface_form: castle peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.3655
lon: -120.349
surface_form: castle peak
instance_of: Mountain
countries: United States
coordinates: lat: 61.597777777778
lon: -143.44361111111
surface_form: castle peak
instance_of: Mountain
countries: United States
coordinates: lat: 44.0396
lon: -114.585
surface_form: castle peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.7731
lon: -106.834
surface_form: castle peak
instance_of: Mountain
countries: United States
coordinates: lat: 46.246388888889
lon: -122.2975
surface_form: castle lake
instance_of: Lake
countries: United States
coordinates: lat: 41.227039
lon: -122.383789
surface_form: castle peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.981944444444
lon: -120.86166666667
surface_form: castle peak
instance_of: Mountain
countries: United States
coordinates: lat: 32.3665
lon: -99.9995
surface_form: castle lake
instance_of: Lake
countries: United States
coordinates: lat: 40.5683
lon: -115.398
surface_form: castle peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.0097
lon: -106.861
Castle Peak is part of the Cascade Range, and it is situated west of Castle Lake. Topographic relief is significant as the summit rises above Castle Lake in one mile. Precipitation runoff from Castle Peak drains into tributaries of the South Fork and the North Fork Toutle River. The nearest higher neighbor is Spud Mountain, to the west-northwest, and Mount St. Helens rises to the southeast.

Geographic entities mentioned:
surface_form: castle peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.3655
lon: -120.349
surface_form: castle peak
instance_of: Mountain
countries: United States
coordinates: lat: 61.597777777778
lon: -143.44361111111
surface_form: castle peak
instance_of: Mountain
countries: United States
coordinates: lat: 44.0396
lon: -114.585
surface_form: castle peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.7731
lon: -106.834
surface_form: castle peak
instance_of: Mountain
countries: United States
coordinates: lat: 46.246388888889
lon: -122.2975
surface_form: castle peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.981944444444
lon: -120.86166666667
surface_form: castle peak
instance_of: Mountain
countries: United States
coordinates: lat: 32.3665
lon: -99.9995
surface_form: castle peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.0097
lon: -106.861
During the Pleistocene period dating back over two million years ago, glaciation advancing and retreating repeatedly scoured and shaped the landscape. With the North American Plate overriding the Pacific Plate, episodes of volcanic igneous activity occurred. The lateral blast from the 1980 eruption of Mount St. Helens was directed toward Castle Peak and stripped the vegetation from the slopes.

Geographic entities mentioned:
surface_form: castle peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.3655
lon: -120.349
surface_form: castle peak
instance_of: Mountain
countries: United States
coordinates: lat: 61.597777777778
lon: -143.44361111111
surface_form: mount st. helens
instance_of: Mountain
countries: United States
coordinates: lat: 46.200277777778
lon: -122.18944444444
surface_form: st. helens
instance_of: Mountain
countries: United States
coordinates: lat: 46.200277777778
lon: -122.18944444444
surface_form: castle peak
instance_of: Mountain
countries: United States
coordinates: lat: 44.0396
lon: -114.585
surface_form: castle peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.7731
lon: -106.834
surface_form: castle peak
instance_of: Mountain
countries: United States
coordinates: lat: 46.246388888889
lon: -122.2975
surface_form: castle peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.981944444444
lon: -120.86166666667
surface_form: castle peak
instance_of: Mountain
countries: United States
coordinates: lat: 32.3665
lon: -99.9995
surface_form: castle peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.0097
lon: -106.861
The lateral blast from the 1980 eruption of Mount St. Helens was directed toward Castle Peak and stripped the vegetation from the slopes. Due to Mount Saint Helens' proximity to Castle Peak, volcanic ash is common in the area. Climate. Castle Peak is located in the marine west coast climate zone of western North America.

Geographic entities mentioned:
surface_form: castle peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.3655
lon: -120.349
surface_form: castle peak
instance_of: Mountain
countries: United States
coordinates: lat: 61.597777777778
lon: -143.44361111111
surface_form: mount saint helens
instance_of: Mountain
countries: United States
coordinates: lat: 46.200277777778
lon: -122.18944444444
surface_form: saint helens
instance_of: Mountain
countries: United States
coordinates: lat: 46.200277777778
lon: -122.18944444444
surface_form: castle peak
instance_of: Mountain
countries: United States
coordinates: lat: 44.0396
lon: -114.585
surface_form: castle peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.7731
lon: -106.834
surface_form: castle peak
instance_of: Mountain
countries: United States
coordinates: lat: 46.246388888889
lon: -122.2975
surface_form: castle peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.981944444444
lon: -120.86166666667
surface_form: castle peak
instance_of: Mountain
countries: United States
coordinates: lat: 32.3665
lon: -99.9995
surface_form: castle peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.0097
lon: -106.861
Helens was directed toward Castle Peak and stripped the vegetation from the slopes. Due to Mount Saint Helens' proximity to Castle Peak, volcanic ash is common in the area. Climate. Castle Peak is located in the marine west coast climate zone of western North America. Most weather fronts originating in the Pacific Ocean travel northeast toward the Cascade Mountains.

Geographic entities mentioned:
surface_form: castle peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.3655
lon: -120.349
surface_form: castle peak
instance_of: Mountain
countries: United States
coordinates: lat: 61.597777777778
lon: -143.44361111111
surface_form: castle peak
instance_of: Mountain
countries: United States
coordinates: lat: 44.0396
lon: -114.585
surface_form: castle peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.7731
lon: -106.834
surface_form: castle peak
instance_of: Mountain
countries: United States
coordinates: lat: 46.246388888889
lon: -122.2975
surface_form: castle peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.981944444444
lon: -120.86166666667
surface_form: castle peak
instance_of: Mountain
countries: United States
coordinates: lat: 32.3665
lon: -99.9995
surface_form: castle peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.0097
lon: -106.861
Castle Peak is a mountain summit in Cowlitz County, Washington, United States. Description. Castle Peak ranks as the third-highest summit in Cowlitz County. It is located on the boundary shared by Mount St. Helens National Volcanic Monument and Gifford Pinchot National Forest. Castle Peak is part of the Cascade Range, and it is situated west of Castle Lake.

Geographic entities mentioned:
surface_form: mount st. helens national volcanic monument
instance_of: Mountain
countries: United States
coordinates: lat: 46.200277777778
lon: -122.18944444444
surface_form: st. helens
instance_of: Mountain
countries: United States
coordinates: lat: 46.200277777778
lon: -122.18944444444
It is located on the boundary shared by Mount St. Helens National Volcanic Monument and Gifford Pinchot National Forest. Castle Peak is part of the Cascade Range, and it is situated west of Castle Lake. Topographic relief is significant as the summit rises above Castle Lake in one mile. Precipitation runoff from Castle Peak drains into tributaries of the South Fork and the North Fork Toutle River.

Geographic entities mentioned:
surface_form: castle lake
instance_of: Lake
countries: United States
coordinates: lat: 41.227039
lon: -122.383789
surface_form: castle lake
instance_of: Lake
countries: United States
coordinates: lat: 40.5683
lon: -115.398
Blanding is a gateway to an abundance of nearby natural and archaeological resources, including The Dinosaur Museum, Natural Bridges National Monument, Monument Valley, and the Four Corners area, Glen Canyon National Recreation Area (Lake Powell), Cedar Mesa archaeological and wilderness area, the San Juan River including Goosenecks State Park, and the Needles district of Canyonlands National Park.

Geographic entities mentioned:
surface_form: Cedar Mesa
instance_of: Landform
countries: United States
coordinates: lat: 37.433
lon: -109.917
Education. The San Juan School District operates Blanding Elementary School, Albert R. Lyman Middle School, and San Juan High School in Blanding. Utah State University has a campus in Blanding. Geography. Blanding is located in the Four Corners area of the Colorado Plateau. According to the United States Census Bureau, the city has a total area of 2.4 square miles (6.1 km2), all land. Climate.

Geographic entities mentioned:
surface_form: Colorado Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 37
lon: -110
Robinson Treaties. The Robinson Treaties are two treaties signed between the Ojibwa chiefs and the Crown in 1850 in the Province of Canada. The first treaty involved Ojibwa chiefs along the north shore of Lake Superior, and is known as the Robinson Superior Treaty.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
The first treaty involved Ojibwa chiefs along the north shore of Lake Superior, and is known as the Robinson Superior Treaty. The second treaty, signed two days later, included Ojibwa chiefs from along the eastern and northern shores of Lake Huron, and is known as the Robinson Huron Treaty. The Wiikwemkoong First Nation did not sign either treaty, and their land is considered &quot;unceded&quot;.

Geographic entities mentioned:
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
Robinson Superior Treaty. The Robinson Treaty for the Lake Superior region, commonly called Robinson Superior Treaty, was entered into agreement on September 7, 1850, at Sault Ste. Marie, Ontario, between Ojibwa Chiefs inhabiting the Northern Shore of Lake Superior from Pigeon River to Batchawana Bay, and The Crown, represented by a delegation headed by William Benjamin Robinson.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
It is registered as the Crown Treaty Number 60. Robinson Huron Treaty. The first Robinson Treaty for the Lake Huron region, commonly called Robinson Huron Treaty, was entered into agreement on September 9, 1850, at Sault Ste. Marie, Ontario, between Ojibwa Chiefs inhabiting the Northern Shore of Lake Superior from Batchawana Bay to Sault Ste.

Geographic entities mentioned:
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
Marie, Ontario, between Ojibwa Chiefs inhabiting the Northern Shore of Lake Superior from Batchawana Bay to Sault Ste. Marie and the Ojibwa Chiefs inhabiting the eastern and northern shores of Lake Huron from Sault Ste. Marie to Penetanguishene, and The Crown, represented by a delegation headed by William Benjamin Robinson. It is registered as the Crown Treaty Number 61.

Geographic entities mentioned:
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
Schultz Glacier. Schultz Glacier () is a glacier flowing east between Pond Peak and Purgatory Peak to join Victoria Lower Glacier. Named by Advisory Committee on Antarctic Names (US-ACAN) for Lieutenant Robert L. Schultz, U.S. Navy, Officer-in-Charge of the Naval Support Force winter-over detachment at McMurdo Station in 1975.

Geographic entities mentioned:
surface_form: Pond Peak
instance_of: Mountain
coordinates: lat: -77.31666667
lon: 162.4
surface_form: Purgatory Peak
instance_of: Mountain
coordinates: lat: -77.35
lon: 162.3
Joshua Wawanosh. Chief Joshua Wawanosh was a First Nations leader of Ojibwe descent, who lived near the southern shore of Lake Huron. He was born near Lake Superior. One source says he had to leave the Lake Superior area after he killed someone. Wawanosh was a leader during the War of 1812. Both his father and grandfather had been hereditary Chiefs, before him. All four of his sons were Chiefs.

Geographic entities mentioned:
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
Joshua Wawanosh. Chief Joshua Wawanosh was a First Nations leader of Ojibwe descent, who lived near the southern shore of Lake Huron. He was born near Lake Superior. One source says he had to leave the Lake Superior area after he killed someone. Wawanosh was a leader during the War of 1812. Both his father and grandfather had been hereditary Chiefs, before him. All four of his sons were Chiefs.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
Oscar-winning producer See-Saw Films (&quot;The King’s Speech&quot;) is producing &quot;Tenzing&quot;, about the inspirational life of Sherpa Tenzing Norgay and his summit of Mount Everest in 1953 alongside fellow outsider New Zealander Edmund Hillary. Balfe will play Jill Henderson, a friend of Tenzing who helped organize trips up Mount Everest. Jennifer Peedom is directing the film.

Geographic entities mentioned:
surface_form: Mount Everest
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.988055555555555
lon: 86.925
Kvamskogen. Kvamskogen (lit. &quot;Kvam forest&quot;) is a mountain plateau in the Hardanger region of Vestland county, Norway. It is located in the municipalities of Samnanger and Kvam. Traditionally, the term was used only for the parts of the plateau located in Kvam municipality, but today it is used for the entire plateau.

Geographic entities mentioned:
surface_form: kvamskogen
instance_of: Plateau
countries: Norway
coordinates: lat: 60.38722222
lon: 5.97166667
She was a &quot;climbing friend&quot; or a &quot;casual sweetheart.&quot; She called him the first friend she had made on her own. When Mallory died on Mount Everest in 1924, Sanders wrote a memoir of him. Her memoir was never published, but it provided much of the material used by later biographers such as David Pye and David Robertson and a novel &quot;Everest Dream&quot;.

Geographic entities mentioned:
surface_form: Mount Everest
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.988055555555555
lon: 86.925
Cone Mountain (Alberta). Cone Mountain is a summit in the Canadian Rockies of Alberta, Canada. It is the southernmost peak in the Sundance Range. Cone Mountain was so named in 1915 on account of its shape. The mountain's name became official in 1924 by the Geographical Names Board of Canada. __NOTOC__
Geology.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: cone mountain (alberta)
instance_of: Mountain
countries: Canada
coordinates: lat: 50.89
lon: -115.46305555555556
Cone Mountain (Alberta). Cone Mountain is a summit in the Canadian Rockies of Alberta, Canada. It is the southernmost peak in the Sundance Range. Cone Mountain was so named in 1915 on account of its shape. The mountain's name became official in 1924 by the Geographical Names Board of Canada. __NOTOC__
Geology.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: cone mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 50.89
lon: -115.46305555555556
Cone Mountain is a summit in the Canadian Rockies of Alberta, Canada. It is the southernmost peak in the Sundance Range. Cone Mountain was so named in 1915 on account of its shape. The mountain's name became official in 1924 by the Geographical Names Board of Canada. __NOTOC__
Geology. The mountain is composed of sedimentary rock laid down during the Precambrian to Jurassic periods.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Cone Mountain was so named in 1915 on account of its shape. The mountain's name became official in 1924 by the Geographical Names Board of Canada. __NOTOC__
Geology. The mountain is composed of sedimentary rock laid down during the Precambrian to Jurassic periods. Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny. Climate.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny. Climate. Based on the Köppen climate classification, Cone Mountain is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below with wind chill factors below.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: cone mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 50.89
lon: -115.46305555555556
Climate. Based on the Köppen climate classification, Cone Mountain is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below with wind chill factors below. Precipitation runoff from Cone Mountain drains into the Bow River which is a tributary of the Saskatchewan River.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: cone mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 50.89
lon: -115.46305555555556
Bungalow side, Old colony and new colony apart from the market area. There is a big railway school and adjacent to it a play ground. Area overview. Purulia district forms the lowest step of the Chota Nagpur Plateau. The general scenario is undulating land with scattered hills. Raghunathpur subdivision occupies the northern part of the district.

Geographic entities mentioned:
surface_form: Chota Nagpur Plateau
instance_of: Plateau
countries: India
coordinates: lat: 23
lon: 85
Wathiyaqucha. Wathiyaqucha (Quechua &quot;wathiya&quot; roasted potatoes, a traditional dish, &quot;qucha&quot; lake, Hispanicized spelling &quot;Bateacocha&quot;) is a mountain in the Andes of Peru. It is situated in the Lima Region, Cajatambo Province, Gorgor District, and in the Huaura Province, Ambar District. Wathiyaqucha lies between Wanki in the west and Puka Parya in the east.

Geographic entities mentioned:
surface_form: Puka Parya
instance_of: Mountain
countries: Peru
coordinates: lat: -10.6783
lon: -77.0244
surface_form: parya
instance_of: Mountain
countries: Peru
coordinates: lat: -13.8056
lon: -74.625
surface_form: parya
instance_of: Mountain
countries: Peru
coordinates: lat: -10.1936
lon: -76.9117
surface_form: puka parya
instance_of: Mountain
countries: Peru
coordinates: lat: -10.6783
lon: -77.0244
surface_form: puka
instance_of: Mountain
countries: Peru
coordinates: lat: -12.6339
lon: -75.5692
Wathiyaqucha. Wathiyaqucha (Quechua &quot;wathiya&quot; roasted potatoes, a traditional dish, &quot;qucha&quot; lake, Hispanicized spelling &quot;Bateacocha&quot;) is a mountain in the Andes of Peru. It is situated in the Lima Region, Cajatambo Province, Gorgor District, and in the Huaura Province, Ambar District. Wathiyaqucha lies between Wanki in the west and Puka Parya in the east.

Geographic entities mentioned:
surface_form: wathiyaqucha
instance_of: Mountain
countries: Peru
coordinates: lat: -10.6775
lon: -77.0408
The town is about 50 km away from Urbino, Jesi, the caves of Frasassi, Senigallia and the Conero coast. Typical products of the Cesano valley are the &quot;Frattula&quot; salami, the &quot;Suasa&quot; onion and many DOC wines as: Verdicchio dei Castelli di Jesi DOC, Rosso Conero DOC, Bianchello del Metauro DOC, Colli Pesaresi DOC, Pergola DOC.

Geographic entities mentioned:
surface_form: Conero coast
instance_of: Mountain
countries: Italy
coordinates: lat: 43.533333333333
lon: 13.6
Fort Stevens (New York). Fort Stevens was a fort on Hallett's Point, Queens, along the East River, constructed in 1814. The fort included a blockhouse on Mill Rock in the River at Hell Gate. Plans from February 1776 showed earlier forts on both sides of the East River including opposite Fort Stevens at Horn's Hook Battery. History.

Geographic entities mentioned:
surface_form: Hell Gate
instance_of: Landform
countries: United States
coordinates: lat: 40.78102
lon: -73.92452
In 1949, he was sent to the United States Naval Academy Preparatory School in anticipation of matriculation at the United States Naval Academy in the fall of 1950. Taking his commission from the USNA in 1954, he served briefly in Flying boats at Willoughby Spit and on board the USS &quot;Arneb&quot; (AKA-56) before entering the Submarine school at Groton, Connecticut.

Geographic entities mentioned:
surface_form: Willoughby Spit
instance_of: Landform
countries: United States
coordinates: lat: 36.967
lon: -76.282472222222
Sauvagella madagascariensis. &quot;Sauvagella madagascariensis&quot; is a small species of fish in the family Clupeidae. It is endemic to fresh and brackish water in rivers of eastern Madagascar, ranging from the Mananjary to the Mananara.

Geographic entities mentioned:
surface_form: Mananjary
instance_of: Watercourse
countries: Madagascar
coordinates: lat: -21.256944444444443
lon: 48.34444444444445
They go skydiving, drive a vintage Shelby Mustang and Dodge Challenger around California Speedway, fly over the North Pole, eat dinner at Chèvre d'or, visit the Taj Mahal, ride motorcycles on the Great Wall of China, attend a lion safari in Tanzania and visit Mount Everest. Atop the Great Pyramid of Giza, they confide mutually about faith and family.

Geographic entities mentioned:
surface_form: Mount Everest
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.988055555555555
lon: 86.925
Brachycorythis kalbreyeri. &quot;Brachycorythis kalbreyeri&quot; is a species of flowering plant in the family Orchidaceae. It is endemic to Equatorial Africa and was first discovered on Mount Cameroon by Guillermo Kalbreyer. It was subsequently named after Kalbreyer by Heinrich Gustav Reichenbach. The species is unique from others in its genus due to its semi-epiphytic growth habit.

Geographic entities mentioned:
surface_form: Mount Cameroon
instance_of: Mountain
countries: Cameroon
coordinates: lat: 4.2166666666667
lon: 9.1725
In addition, effects of xenon on erythropoietin production in humans have not been demonstrated, so far. In 2025, four UK mountaineers, including Alistair Carns, climbed Mount Everest in an expedition lasting only one week, claiming their inhalation of xenon gas to stimulate erythropoietin production had obviated the usual several weeks' altitude acclimatisation.

Geographic entities mentioned:
surface_form: Mount Everest
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.988055555555555
lon: 86.925
The glacier is a famous tourist attraction. Most people who visit the town of Odda usually take the walk to Buarbreen (a part of Folgafonna). The melt-water from this glacier is bottled at source to form the product Isklar. The melt-water also goes down the river from Buarbreen down into the lake Sandvinvatnet. Name.

Geographic entities mentioned:
surface_form: Sandvinvatnet
instance_of: Lake
countries: Norway
coordinates: lat: 60.034444444444
lon: 6.5541666666667
Pic du Mascarin. Geography. This high peak rises above the Lac Perdu and the L'au-delà Plateau in the southern sector of Île de la Possession, the largest island of the Crozet group. The mountain was named after the &quot;Mascarin&quot;, the ship on which French explorers Marc-Joseph Marion du Fresne and his second-in-command Julien Crozet were the first to explore the Crozet Islands in 1772.

Geographic entities mentioned:
surface_form: pic du mascarin
instance_of: Mountain
countries: France
coordinates: lat: -46.4378
lon: 51.7457
The earliest depictions of bells used for livestock in Britain appear on Pictish carved stones of the 7th to 9th centuries AD at Eassie, Angus and Fowlis Wester, Perthshire. Small iron bells of 8th or 9th century date, argued to be for cow or sheep, have been excavated from upland farm settlements at Crummack Dale and Gauber High Pasture in the Yorkshire Dales.

Geographic entities mentioned:
surface_form: Crummack Dale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.141
lon: -2.343
The legend of the Simmental tells how a young cowherd strays inside a mountain, and is offered by a beautiful woman the choice between a treasure of gold coins, a golden Trychel, or the fairy herself. He chooses the Trychel. As opposed to regular cast-metal bells, 'trychlen' are made of hammered sheet metal.

Geographic entities mentioned:
surface_form: Simmental
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.55
lon: 7.36
Sleeping Giant (film). &quot;Sleeping Giant&quot; is a 2015 Canadian drama film written and directed by Andrew Cividino. The film follows three teenage boys coping with boredom in cottage country on the shores of Lake Superior. The film premiered in the Critics' Week section at the 2015 Cannes Film Festival.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
His brother Fred sought to succeed him as mayor, but was unsuccessful. Harless served as a member of the People's Party, of which he was also a former chairman. During his tenure, he oversaw the March 1963 flood that impacted the area, leading him to argue in favor of the Justice Reservoir before the House Committee on Appropriations of the United States Congress.

Geographic entities mentioned:
surface_form: Justice Reservoir
instance_of: Lake
countries: United States
coordinates: lat: 37.6
lon: -81.8222
Harless was a supporter of several major infrastructure initiatives in southern West Virginia, including the Justice Dam, the Hatfield–McCoy Trails, a 225-acre housing development and shopping centre complex on a mountaintop outside his hometown, as well as the King Coal Highway.

Geographic entities mentioned:
surface_form: Justice Dam
instance_of: Lake
countries: United States
coordinates: lat: 37.6
lon: -81.8222
In the Northwest Annual Exhibition of 1935 he won the Katherine Baker Purchase Award, and the museum mounted a solo exhibition of his work the following year. In 1937, Anderson helped refurbish a burned-out house Morris Graves had discovered near the small town of La Conner, Washington, in the Skagit Valley, about sixty miles north of Seattle.

Geographic entities mentioned:
surface_form: Skagit Valley
instance_of: Valley
countries: United States
coordinates: lat: 48.5
lon: -122.033
The site today. The site, on the dip slope of Cranborne Chase, is now part of the Kingston Lacy estate owned by the National Trust since 1982, with free access. The hillfort has been a scheduled ancient monument since 1924. On a clear day, the Isle of Wight is visible from the top.

Geographic entities mentioned:
surface_form: Cranborne Chase
instance_of: Plateau
countries: United Kingdom
coordinates: lat: 50.961419444444
lon: -2.0440888888889
The Vaaluteru gets its name from the Telugu words Vaalu (its shape) and Eeru (stream) which later came to be Waltair. These together make up the Meghadri &quot;Gedda&quot; (drain) which joins the Bay of Bengal at the Dolphin Hill near Visakhapatnam Port. The construction of the dam and the development of Airport and the Harbour has dried up several streams which used to pass through the city.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
Academics. A total of 27 AP classes were offered in the 2015–2016 school year. Facilities. The 26-acre campus is located on the Indian River Lagoon. School facilities include an 800-seat theater, a water complex, two gyms, two libraries, fine arts center with music and arts studios, athletic playing fields, and eight science labs.

Geographic entities mentioned:
surface_form: Indian River Lagoon
instance_of: Body of water
countries: United States
coordinates: lat: 28.05527778
lon: -80.57611111
Geology and topography. The floodplain of Johnson Creek is a remnant of large glacial floods known as the Missoula Floods that deposited thick sediments between 18,000 and 13,000 years ago in the Columbia River Basin, including much of the Willamette Valley. Underlying the sediments are substantial thicknesses of basalt lavas from the Columbia River Basalt Group.

Geographic entities mentioned:
surface_form: Willamette Valley
instance_of: Valley
countries: United States
coordinates: lat: 44.9
lon: -123.1
surface_form: johnson creek
instance_of: Watercourse
countries: United States
coordinates: lat: 45.4442
lon: -122.643
Slopes in the watershed range generally between 1 and 25 percent. Mount Scott and Powell Butte rise to about and have slopes ranging from 10 to 30 percent. Gresham Butte and Hogan Butte, in Gresham, have the steepest slopes, including a few around 50 percent. The Boring Hills, of volcanic origin, rise more than higher than the terraces to the north and west.

Geographic entities mentioned:
surface_form: Powell Butte
instance_of: Mountain
countries: United States
coordinates: lat: 45.487347222222
lon: -122.50179722222
surface_form: mount scott
instance_of: Mountain
countries: United States
coordinates: lat: 45.4545
lon: -122.551
surface_form: mount scott
instance_of: Mountain
countries: United States
coordinates: lat: 47.84092
lon: -123.52991
surface_form: mount scott
instance_of: Mountain
countries: United States
coordinates: lat: 42.923611111111
lon: -122.01472222222
surface_form: mount scott
instance_of: Mountain
countries: United States
coordinates: lat: 34.7445
lon: -98.532
Formed by the ancestral Columbia and Willamette Rivers, the terraces north of Johnson Creek are generally underlain by permeable sand and gravel. Three isolated hills—Rocky Butte, Mount Tabor, and Kelly Butte—rise about above the surrounding terraces.

Geographic entities mentioned:
surface_form: Rocky Butte
instance_of: Mountain
countries: United States
coordinates: lat: 45.546713888889
lon: -122.56594166667
surface_form: kelly butte
instance_of: Mountain
countries: United States
coordinates: lat: 47.169166666667
lon: -121.49027777778
Three isolated hills—Rocky Butte, Mount Tabor, and Kelly Butte—rise about above the surrounding terraces. Except for Powell Butte, the terrain on the creek's north side is less steep than on the south side, which includes Mount Scott and the Boring Lava Domes.

Geographic entities mentioned:
surface_form: mount scott
instance_of: Mountain
countries: United States
coordinates: lat: 45.4545
lon: -122.551
surface_form: mount scott
instance_of: Mountain
countries: United States
coordinates: lat: 47.84092
lon: -123.52991
surface_form: mount scott
instance_of: Mountain
countries: United States
coordinates: lat: 42.923611111111
lon: -122.01472222222
surface_form: powell butte
instance_of: Mountain
countries: United States
coordinates: lat: 45.487347222222
lon: -122.50179722222
surface_form: mount scott
instance_of: Mountain
countries: United States
coordinates: lat: 34.7445
lon: -98.532
Neighboring watersheds on the east side of the Willamette River include Mount Scott Creek and Kellogg Creek, which flow through Milwaukie and drain directly into the Willamette; the Clackamas River, which drains the southeast suburbs and empties into the Willamette near Oregon City; the Sandy River, which drains the eastern suburbs and empties into the Columbia; and Fairview Creek and the Columbia Slough, which drain north Portland and Gresham, emptying into the Columbia.

Geographic entities mentioned:
surface_form: mount scott
instance_of: Mountain
countries: United States
coordinates: lat: 45.4545
lon: -122.551
surface_form: mount scott
instance_of: Mountain
countries: United States
coordinates: lat: 47.84092
lon: -123.52991
surface_form: mount scott
instance_of: Mountain
countries: United States
coordinates: lat: 42.923611111111
lon: -122.01472222222
surface_form: mount scott
instance_of: Mountain
countries: United States
coordinates: lat: 34.7445
lon: -98.532
surface_form: kellogg creek
instance_of: Watercourse
countries: United States
coordinates: lat: 37.90694444444444
lon: -121.60944444444445
The floods primarily affect four areas in Portland: Tideman Johnson Natural Area at Southeast 45th Avenue, the area west of Southeast 82nd Avenue; Lents, and lower Powell Butte. The U.S. National Weather Service defines Johnson Creek's flood stage, measured at USGS station 14211500 at Sycamore in Portland, as, equivalent to a flow rate (discharge rate) of about per second.

Geographic entities mentioned:
surface_form: johnson creek
instance_of: Watercourse
countries: United States
coordinates: lat: 45.4442
lon: -122.643
Erosion is not a big threat in the northwestern part of the watershed, where the land is flat and developed, or in the northeast, dominated by low-erosion soils. In the southeast, soils have a medium risk of erosion, and soils around Powell Butte and the Boring Lava Domes have &quot;an extremely high erodibility factor and are sensitive to ground disturbance&quot;.

Geographic entities mentioned:
surface_form: powell butte
instance_of: Mountain
countries: United States
coordinates: lat: 45.487347222222
lon: -122.50179722222
The airport, at about above sea level, is at essentially the same elevation as the mouth of Johnson Creek. Annual precipitation at higher elevations in the creek's upper watershed is much greater, more than. The floods primarily affect four areas in Portland: Tideman Johnson Natural Area at Southeast 45th Avenue, the area west of Southeast 82nd Avenue; Lents, and lower Powell Butte. The U.S.

Geographic entities mentioned:
surface_form: powell butte
instance_of: Mountain
countries: United States
coordinates: lat: 45.487347222222
lon: -122.50179722222
Creekside parks include Johnson Creek Park, about of natural areas and paths; the Crystal Springs Rhododendron Garden, along Crystal Springs Creek; Tideman Johnson Natural Area, about of natural areas and paths; Leach Botanical Garden, about, a public garden dedicated to the study of botany and horticulture with an emphasis on plants of the Pacific Northwest; Beggars Tick Wildlife Refuge, a wetland of; Foster Floodplains Natural Area, a reclaimed floodplain in area; Powell Butte Nature Park, about on an extinct cinder cone volcano, including natural areas and hiking, biking, and equestrian trails; and Gresham's Main City Park, about including sports fields, picnic areas, and trails.

Geographic entities mentioned:
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instance_of: Mountain
countries: United States
coordinates: lat: 45.487347222222
lon: -122.50179722222
surface_form: cinder cone
instance_of: Mountain
countries: United States
coordinates: lat: 40.547386111111
lon: -121.31997222222
In 2007, Metro bought two parcels of land totaling for preservation adjacent to Johnson Creek on Clatsop Butte, south of Foster Road near Powell Butte and Portland's Pleasant Valley neighborhood. The purchases cost $10.9 million, drawing on bonds approved by a 2006 ballot measure. They were praised by conservationists but questioned by others who thought Metro had paid too much.

Geographic entities mentioned:
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instance_of: Mountain
countries: United States
coordinates: lat: 45.487347222222
lon: -122.50179722222
surface_form: pleasant valley
instance_of: Valley
countries: United States
coordinates: lat: 39.6389
lon: -77.5472
surface_form: pleasant valley
instance_of: Valley
countries: United States
coordinates: lat: 39.6409256
lon: -114.0184307
surface_form: johnson creek
instance_of: Watercourse
countries: United States
coordinates: lat: 45.4442
lon: -122.643
The watershed is a roughly rectangular area of about. The topography of the watershed varies greatly from the high point of about above sea level in the Boring Hills near the creek's source to the low point of where the creek meets the Willamette River. Slopes in the watershed range generally between 1 and 25 percent.

Geographic entities mentioned:
surface_form: high point
instance_of: Mountain
countries: United States
coordinates: lat: 41.924722222222
lon: -74.288055555556
surface_form: high point
instance_of: Mountain
countries: United States
coordinates: lat: 41.3209
lon: -74.6616
As the creek descends, so do the avenue numbers. The creek begins in uplands in Clackamas County east of Southeast 362nd Avenue and flows swiftly to the west for about, crisscrossing the border between Clackamas County and Multnomah County 5 times in this upstream stretch, and passing under U.S. Route 26, the Mount Hood Highway, in Multnomah County at about from the mouth.

Geographic entities mentioned:
surface_form: mount hood
instance_of: Mountain
countries: United States
coordinates: lat: 38.4599
lon: -122.553
surface_form: mount hood
instance_of: Mountain
countries: United States
coordinates: lat: 45.37361111111111
lon: -121.69583333333334
surface_form: hood
instance_of: Mountain
countries: United States
coordinates: lat: 45.37361111111111
lon: -121.69583333333334
Shortly thereafter, Johnson Creek passes the USGS gauge station at Sycamore, from the mouth, and flows under Cedar Crossing Bridge. Meandering slowly through the Lents neighborhood of Portland, Johnson Creek receives Veterans Creek, which enters on the left from its headwaters in Happy Valley in Clackamas County.

Geographic entities mentioned:
surface_form: happy valley
instance_of: Valley
countries: United States
coordinates: lat: -14.279722222222
lon: -170.69638888889
surface_form: johnson creek
instance_of: Watercourse
countries: United States
coordinates: lat: 45.4442
lon: -122.643
Jurisdiction. Six local political jurisdictions overlap with the Johnson Creek watershed. In 2000, 38 percent of the watershed was in Portland's city limits, 24 percent in unincorporated Clackamas County, 23 percent in Gresham, 11 percent in unincorporated Multnomah County, 4 percent in Milwaukie, and 0.1 percent in Happy Valley. None of the cities lies entirely within the watershed.

Geographic entities mentioned:
surface_form: happy valley
instance_of: Valley
countries: United States
coordinates: lat: -14.279722222222
lon: -170.69638888889
None of the cities lies entirely within the watershed. In 2000, Johnson Creek and its tributaries drained 53 percent of Gresham, 42 percent of Milwaukie, 19 percent of Happy Valley, and 14 percent of Portland. The watershed covered only 1.2 percent of unincorporated Multnomah County and less than 1 percent of unincorporated Clackamas County.

Geographic entities mentioned:
surface_form: happy valley
instance_of: Valley
countries: United States
coordinates: lat: -14.279722222222
lon: -170.69638888889
In 1903, the Springwater Division Line, also known as the Portland Traction Company Line, the Cazadero Line, and the Bellrose Line, was built along Johnson Creek to provide rail transport for passengers and freight. Sellwood, Eastmoreland, Lents, and Pleasant Valley were among the new communities that grew up along the line. By the 1920s, housing began to replace creekside farms.

Geographic entities mentioned:
surface_form: pleasant valley
instance_of: Valley
countries: United States
coordinates: lat: 39.6389
lon: -77.5472
surface_form: pleasant valley
instance_of: Valley
countries: United States
coordinates: lat: 39.6409256
lon: -114.0184307
By 2,000 to 3,000 years ago, settlements in the Clackamas River basin, adjacent to the Johnson Creek watershed, had moved to the river's lower floodplain. The area was the home of the Clackamas Indians, a subgroup of the Chinookan speakers who lived in the Columbia River Valley from Celilo Falls to the Pacific Ocean.

Geographic entities mentioned:
surface_form: river valley
instance_of: Valley
countries: United States
coordinates: lat: 35.36
lon: -93.37
Johnson Creek (Willamette River tributary). Johnson Creek is a tributary of the Willamette River in the Portland metropolitan area of the U.S. state of Oregon. Part of the drainage basin of the Columbia River, its catchment consists of of mostly urban land occupied by about 180,000 people as of 2012.

Geographic entities mentioned:
surface_form: johnson creek (willamette river tributary)
instance_of: Watercourse
countries: United States
coordinates: lat: 45.4442
lon: -122.643
Johnson Creek (Willamette River tributary). Johnson Creek is a tributary of the Willamette River in the Portland metropolitan area of the U.S. state of Oregon. Part of the drainage basin of the Columbia River, its catchment consists of of mostly urban land occupied by about 180,000 people as of 2012.

Geographic entities mentioned:
surface_form: johnson creek
instance_of: Watercourse
countries: United States
coordinates: lat: 45.4442
lon: -122.643
As urban density increased in the floodplain, seasonal floods grew more damaging. In the 1930s the Works Progress Administration of the federal government lined the lower of Johnson Creek with rock to control the floods. Despite this, the creek flooded 37 times between 1941 and 2006.

Geographic entities mentioned:
surface_form: johnson creek
instance_of: Watercourse
countries: United States
coordinates: lat: 45.4442
lon: -122.643
Since the 1990s, regional planners have tried to reduce flooding by controlling stormwater runoff, creating stream meanders, reducing erosion, replacing impervious surfaces, and protecting riparian buffers. The Johnson Creek watershed includes the subwatersheds of Badger Creek, Sunshine Creek, Kelley Creek, Mitchell Creek, Veterans Creek, Crystal Springs Creek, and smaller streams.

Geographic entities mentioned:
surface_form: johnson creek
instance_of: Watercourse
countries: United States
coordinates: lat: 45.4442
lon: -122.643
Course. Johnson Creek begins near the unincorporated community of Cottrell in Clackamas County, Oregon, southeast of Gresham in the foothills of the Cascade Range, and flows generally westward about to its confluence with the Willamette River, a major tributary of the Columbia River.

Geographic entities mentioned:
surface_form: johnson creek
instance_of: Watercourse
countries: United States
coordinates: lat: 45.4442
lon: -122.643
Route 26, the Mount Hood Highway, in Multnomah County at about from the mouth. Shortly thereafter, it receives Badger Creek and Sunshine Creek from the left and the North Fork of Johnson Creek from the right.

Geographic entities mentioned:
surface_form: johnson creek
instance_of: Watercourse
countries: United States
coordinates: lat: 45.4442
lon: -122.643