Sarmila/GeoWiki-Features huggingface dataset:
Goose Eye Mountain. Goose Eye Mountain, also known as Mt. Goose High, is a mountain located in Oxford County, Maine, about. (2 km) east of the New Hampshire-Maine border. The mountain is the second-highest peak of the Mahoosuc Range of the White Mountains. Description. Goose Eye Mountain is flanked to the northeast by Fulling Mill Mountain, and to the southwest by Mount Carlo.

Geographic entities mentioned:
surface_form: goose eye mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.502558333333
lon: -70.991463888889
Description. Goose Eye Mountain is flanked to the northeast by Fulling Mill Mountain, and to the southwest by Mount Carlo. Goose Eye Mountain stands within the watershed of the Androscoggin River, which wraps around the Mahoosuc Range and drains into Merrymeeting Bay, the estuary of the Kennebec River, and then into the Gulf of Maine.

Geographic entities mentioned:
surface_form: goose eye mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.502558333333
lon: -70.991463888889
It has an area of and a total population of about 344,000 in 36 &quot;comuni&quot; (: &quot;comune&quot;). The north of the province of Arezzo contains the Pratomagno and Casentino mountain ranges and valleys, and the southern areas of the region contain the fertile Tiber and Chiana valleys.

Geographic entities mentioned:
surface_form: Pratomagno
instance_of: Mountain
countries: Italy
coordinates: lat: 43.65
lon: 11.65
surface_form: Casentino
instance_of: Valley
countries: Italy
coordinates: lat: 43.7
lon: 11.816666666667
An on-site warden at the park leads small groups on foot to find the Chillingham cattle herd; on some days they are evident in one of the easily accessible meadows, while on rare occasions they can be difficult to find without a fair bit of walking, given the tangled woodlands and the amount of space they have for roaming. Just to the east of the park is the summit of Ros Hill.

Geographic entities mentioned:
surface_form: Ros Hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 55.521380555556
lon: -1.8732694444444
Rome Hill. Rome Hill, also called St. Davids Hill, is a small summit at the southwest corner of Lake Elsinore. It lies at an elevation of.

Geographic entities mentioned:
surface_form: Lake Elsinore
instance_of: Lake
countries: United States
coordinates: lat: 33.660069444444
lon: -117.35183888889
The Dubois Museum preserves and interprets the natural and social history of the Upper Wind River Valley as the National Bighorn Sheep Interpretive Center focuses on public education about the biology and habitat of the Rocky Mountain Bighorn Sheep with focus on the largest herd of Rocky Mountain Bighorn sheep in the coterminous United States that winter in the Whiskey Basin of Whiskey Mountain adjacent to the Fitzpatrick Wilderness in the Shoshone National Forest.

Geographic entities mentioned:
surface_form: Whiskey Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.4303
lon: -109.623
Bera Lake. Bera Lake (Malay: &quot;Tasik Bera&quot;; Chinese: 比拉湖) is a natural freshwater lake system, located in Bera District, Pahang, Malaysia in the saddle of the main and eastern mountain ranges of Peninsular Malaysia, extending 35 km long and 20 km wide, drainings into the Pahang River. It lends its name to the Bera district and parliamentary constituency.

Geographic entities mentioned:
surface_form: tasik bera
instance_of: Lake
countries: Malaysia
coordinates: lat: 3.8166666666667
lon: 102.41666666667
surface_form: bera lake
instance_of: Lake
countries: Malaysia
coordinates: lat: 3.8166666666667
lon: 102.41666666667
It lends its name to the Bera district and parliamentary constituency. As the largest freshwater swamp in Peninsular Malaysia, Tasik Bera or Bera Lake remains both a unique and remote wetland wilderness. Surrounded by a patchwork of dry lowland dipterocarp forests, the lake environment includes islands of peat swamp forests.

Geographic entities mentioned:
surface_form: tasik bera
instance_of: Lake
countries: Malaysia
coordinates: lat: 3.8166666666667
lon: 102.41666666667
surface_form: bera lake
instance_of: Lake
countries: Malaysia
coordinates: lat: 3.8166666666667
lon: 102.41666666667
Bera Lake. Bera Lake (Malay: &quot;Tasik Bera&quot;; Chinese: 比拉湖) is a natural freshwater lake system, located in Bera District, Pahang, Malaysia in the saddle of the main and eastern mountain ranges of Peninsular Malaysia, extending 35 km long and 20 km wide, drainings into the Pahang River. It lends its name to the Bera district and parliamentary constituency.

Geographic entities mentioned:
surface_form: bera lake
instance_of: Lake
countries: Malaysia
coordinates: lat: 3.8166666666667
lon: 102.41666666667
California State Route 269. State Route 269 (SR 269) is a state highway in the U.S. state of California. It runs in the San Joaquin Valley from State Route 33 in Avenal to State Route 145 in the community of Five Points. Route description. The southern terminus of SR 269 is at State Route 33 in Avenal. In the city of Avenal, it is known as Skyline Boulevard.

Geographic entities mentioned:
surface_form: San Joaquin Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.628888888889
lon: -120.185
Route description. The southern terminus of SR 269 is at State Route 33 in Avenal. In the city of Avenal, it is known as Skyline Boulevard. It crosses the Kettleman Hills and drops into the San Joaquin Valley at I-5. From the Fresno-Kings county line, right before I-5 to its northern terminus at SR 145, the road is known as Lassen Avenue and heads due north through Huron.

Geographic entities mentioned:
surface_form: San Joaquin Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.628888888889
lon: -120.185
Sesquilé. Sesquilé is a town and municipality in Almeidas Province in the department of Cundinamarca, Colombia. Sesquilé in the Chibcha language of the Muisca means &quot;hot water&quot;. Sesquilé is adjacent to Tominé Reservoir and nearby Lake Guatavita, the suspected site of the &quot;El Dorado&quot; legend.

Geographic entities mentioned:
surface_form: Tominé Reservoir
instance_of: Lake
countries: Colombia
coordinates: lat: 4.954
lon: -73.84
surface_form: Lake Guatavita
instance_of: Lake
countries: Colombia
coordinates: lat: 4.9772222222222
lon: -73.775555555556
Saddleworth is a civil parish of the Metropolitan Borough of Oldham in Greater Manchester, England. It comprises several villages and hamlets amongst the west side of the Pennine hills: Uppermill, Greenfield, Dobcross, Delph, Diggle and others. Saddleworth lies to the east of the large town of Oldham.

Geographic entities mentioned:
surface_form: west side
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.543333333333
lon: -1.9558333333333
In 1858, Parker accepted a position as a school teacher in Bloomington, Indiana. He took a similar position in Pike County, Missouri, after one term. During the summer of 1859, he traveled with an ox cart to the Pikes Peak area near the present location of Denver, Colorado. After a summer of prospecting he returned to his teaching position in Missouri.

Geographic entities mentioned:
surface_form: Pikes Peak
instance_of: Mountain
countries: United States
coordinates: lat: 38.840555555556
lon: -105.04416666667
Geography. The park is located at the western end of Seton Portage between Seton Portage Road to the southeast, and a pair of railway tracks owned by CN Rail to the northwest. The Seton River lies just beyond the railway tracks, which flows northwest from Anderson Lake into Seton Lake. The park is forested with pine and the light underbrush typical of the area's climate.

Geographic entities mentioned:
surface_form: Seton Lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.7
lon: -122.167
Toluca Lake, Los Angeles. Toluca Lake is a neighborhood in the city of Los Angeles, California, located in the San Fernando Valley northwest of downtown. The name is also given to a private natural lake fed by wells and maintained by neighboring property owners. Prior to the paving of the Los Angeles River in 1938 and L.A.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
Early years. The Tongva people have lived in the San Fernando Valley and the Los Angeles basin for 8,000 years. The Tongvan settlement Cahuenga used the springs and marsh in the Toluca Lake locale for water, fishing, hunting, harvesting, and building supplies (tule plants).

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
The Tongvan settlement Cahuenga used the springs and marsh in the Toluca Lake locale for water, fishing, hunting, harvesting, and building supplies (tule plants). After the Spanish conquest in the 1790s of Las Californias, the San Fernando Valley, including the &quot;Toluca Lake locale&quot;, became the extended property of the Mission San Fernando Rey de España.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
In June 2018, Ron Burkle purchased the 5.2 acre Bob Hope estate for $15 million, with the proceeds going to the Bob and Dolores Hope Foundation. In 2021, Kelly Clarkson purchased an original 1936 colonial-style mansion on a Toluca Lake property. Community. The Toluca Lake neighborhood is situated on of the southeastern San Fernando Valley. The Mapping L.A.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
Chalía River. The Chalía River is a river of Argentina.

Geographic entities mentioned:
surface_form: chalía river
instance_of: Watercourse
countries: Argentina
coordinates: lat: -49.59356
lon: -69.51352
Qiwllaqucha (Quechua &quot;qillwa, qiwlla, qiwiña&quot; gull, &quot;qucha&quot; lake, &quot;gull lake&quot;, Hispanicized names &quot;Lago Quiula, Laguna Quiula&quot;) is a lake at an unpopulated place of that name &quot;(Quiulacocha)&quot; in Peru located in the Lima Region, Huarochirí Province, Laraos District. Qiwllaqucha lies in the north of the district, southeast of Raqray.

Geographic entities mentioned:
surface_form: Raqray
instance_of: Mountain
countries: Peru
coordinates: lat: -11.47
lon: -76.475
surface_form: raqray
instance_of: Mountain
countries: Peru
coordinates: lat: -11.47
lon: -76.475
Qiwllaqucha (Huarochirí). Qiwllaqucha (Quechua &quot;qillwa, qiwlla, qiwiña&quot; gull, &quot;qucha&quot; lake, &quot;gull lake&quot;, Hispanicized names &quot;Lago Quiula, Laguna Quiula&quot;) is a lake at an unpopulated place of that name &quot;(Quiulacocha)&quot; in Peru located in the Lima Region, Huarochirí Province, Laraos District.

Geographic entities mentioned:
surface_form: qiwllaqucha
instance_of: Mountain
countries: Peru
coordinates: lat: -10.03527778
lon: -76.38638889
surface_form: qiwllaqucha
instance_of: Lake
Mountain
countries: Peru
coordinates: lat: -12.85833333
lon: -74.98888889
surface_form: qiwllaqucha
instance_of: Mountain
countries: Peru
coordinates: lat: -13.1381
lon: -74.7617
surface_form: qiwllaqucha
instance_of: Mountain
countries: Peru
coordinates: lat: -11.96694444
lon: -75.82805556
surface_form: qiwllaqucha (huarochirí)
instance_of: Lake
countries: Peru
coordinates: lat: -11.476666666667
lon: -76.485833333333
Qiwllaqucha (Huarochirí). Qiwllaqucha (Quechua &quot;qillwa, qiwlla, qiwiña&quot; gull, &quot;qucha&quot; lake, &quot;gull lake&quot;, Hispanicized names &quot;Lago Quiula, Laguna Quiula&quot;) is a lake at an unpopulated place of that name &quot;(Quiulacocha)&quot; in Peru located in the Lima Region, Huarochirí Province, Laraos District.

Geographic entities mentioned:
surface_form: qiwllaqucha
instance_of: Mountain
countries: Peru
coordinates: lat: -10.03527778
lon: -76.38638889
surface_form: qiwllaqucha
instance_of: Mountain
countries: Peru
coordinates: lat: -10.03527778
lon: -76.38638889
surface_form: qiwllaqucha
instance_of: Lake
Mountain
countries: Peru
coordinates: lat: -12.85833333
lon: -74.98888889
surface_form: qiwllaqucha
instance_of: Lake
Mountain
countries: Peru
coordinates: lat: -12.85833333
lon: -74.98888889
surface_form: quiulacocha
instance_of: Lake
Mountain
countries: Peru
coordinates: lat: -12.85833333
lon: -74.98888889
surface_form: qiwllaqucha
instance_of: Mountain
countries: Peru
coordinates: lat: -13.1381
lon: -74.7617
surface_form: qiwllaqucha
instance_of: Mountain
countries: Peru
coordinates: lat: -13.1381
lon: -74.7617
surface_form: qiwllaqucha
instance_of: Mountain
countries: Peru
coordinates: lat: -11.96694444
lon: -75.82805556
surface_form: qiwllaqucha
instance_of: Mountain
countries: Peru
coordinates: lat: -11.96694444
lon: -75.82805556
surface_form: qiwllaqucha
instance_of: Lake
countries: Peru
coordinates: lat: -11.476666666667
lon: -76.485833333333
surface_form: qiwllaqucha
instance_of: Lake
countries: Peru
coordinates: lat: -11.476666666667
lon: -76.485833333333
surface_form: laguna quiula
instance_of: Lake
countries: Peru
coordinates: lat: -11.476666666667
lon: -76.485833333333
She is running for re-election. District 3. The 3rd district is located in the western San Fernando Valley, bordering Ventura County and including the neighborhoods of Woodland Hills, Tarzana, Reseda, Winnetka and Canoga Park. The incumbent councilor is Bob Blumenfield, who was first elected in 2013. Blumenfield is term-limited cannot seek re-election to office. District 5.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
The incumbent is Katy Yaroslavsky, who was first elected in 2022 after defeating Sam Yebri. District 7. The 7th district is located in the northern San Fernando Valley and includes the neighborhoods of Sylmar, Lake View Terrace, Sunland-Tujunga, Pacoima, Arleta and Mission Hills. The incumbent is Monica Rodriguez, who was first elected in 2017 and re-elected in 2022. District 11.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
Toronto Islands. The Toronto Islands are a chain of 15 small islands in Lake Ontario, south of mainland Toronto, Ontario, Canada. Comprising the only group of islands in the western part of Lake Ontario, the Toronto Islands are located just offshore from the city's downtown area, provide shelter for Toronto Harbour, and separate Toronto from the rest of Lake Ontario.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
Hanlan's Point Beach is an officially recognized nude beach, one of only two in Canada. Ward's Island Beach is located on the island east end near the Eastern Gap. Centre Island Beach is located on the south side of the island and faces out to Lake Ontario. The beach is actually two beaches with the portion west of the Lookout Pier called Manitou Beach.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
In the same place the post-Byzantine church of the Slumber of Virgin Mary is located. Modern history. Several residents from Kontariotissa took part in the Revolution of Olympus, in 1878, against Turks. Many European travellers visited the settlement.

Geographic entities mentioned:
surface_form: Olympus
instance_of: Mountain
countries: Greece
coordinates: lat: 40.083333333333336
lon: 22.35
He began to do fieldwork in anthropology in 1929 but his work was often contested due to his lack of credentials. In 1945, at the age of 42, he finally obtained a doctorate under the direction of Marcel Griaule. He led unsuccessful expeditions to Hoggar and Teffedest Mountains in 1949–1950. Discovery of Tassili.

Geographic entities mentioned:
surface_form: Hoggar
instance_of: Plateau
countries: Algeria
France
coordinates: lat: 23.288611
lon: 5.534167
Banitsa (ruins). Banitsa (– Karié, Bulgarian/Macedonian: Баница, &quot;Banitsa&quot; or &quot;Banica&quot;, Ottoman Turkish: &quot;بانيچه&quot; Turkish &quot;Baniçe&quot;) is a deserted village in Serres regional unit, northern Greece. Its ruins are situated some 15 km north-east of the town of Serres, near the present-day village of Oreini, on the southern slopes of the Vrontous mountains.

Geographic entities mentioned:
surface_form: Vrontous
instance_of: Mountain
countries: Greece
coordinates: lat: 41.258
lon: 23.602
In contrast, the climate in the eastern and southern regions is less conducive to breeding. As a result, most horses are bred along the Rhine Valley. Germany has 9 federal stud farms (), financed and managed by the federal states (), which organize the breeding on a regional level, particularly by supporting and promoting horse breeds specific to each state.

Geographic entities mentioned:
surface_form: Rhine Valley
instance_of: Valley
Cowgirl Creamery. Cowgirl Creamery is a company located in Petaluma, California, which manufactures artisan cheeses. Founded in 1994, the company manufactures its own cheeses and sells other imported and domestic cheese and fine artisan foods. Its own cheeses include &quot;Red Hawk&quot; and &quot;Mt. Tam&quot; (named after Mount Tamalpais).

Geographic entities mentioned:
surface_form: Mount Tamalpais
instance_of: Mountain
countries: United States
coordinates: lat: 37.9291
lon: -122.578
Their aged cheeses are named after landmarks or other features local to the Marin Headlands. Cowgirl Creamery also makes fresh cheeses: a fromage blanc and a crème fraiche and recently resumes making their clabbered cottage cheese; they no longer make Niloufer's Panir (which is named for chef Niloufer Ichaporia King). History. The company was started in 1994.

Geographic entities mentioned:
surface_form: Marin Headlands
instance_of: Landform
countries: United States
coordinates: lat: 37.827777777778
lon: -122.50611111111
It lies just off the A48 road, 7 miles north west of Ammanford and 9 miles north of Llanelli. Its nearby community villages include Cross Hands, Drefach, Cwmmawr, Foelgastell and Gorslas. The Gwendraeth Fawr river flows nearby and its source is at Llyn Llech Owain, just north of the village. Cefneithin has a chapel (Tabernacl), a village hall (Y Neuadd), a primary school, and a secondary school.

Geographic entities mentioned:
surface_form: Llyn Llech Owain
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.816
lon: -4.078
Large investigations have focused on the conterminous US (e.g. the National Science Foundation EarthScope MT Program and its successor NASA and USGS MTArray), the East Pacific Rise, Australia (AusLAMP MT Program), Southern Africa (SAMTEX MT Project), China (Part of the Sinoprobe project) and the Tibetan Plateau. Earthquake precursor prediction.

Geographic entities mentioned:
surface_form: Tibetan Plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 33
lon: 88
Hanna Venture Base, located near Akela's World, is the smallest part of the Crystal Lake Scout Reservation. It was named after, and financially supported by Al Hanna, whose achievements include climbing to the top of Mount Everest. The hub for Venturing in Samoset Council, it features an indoor climbing wall and an outdoor 60’ climbing tower, with walls for rappelling and climbing.

Geographic entities mentioned:
surface_form: Mount Everest
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.988055555555555
lon: 86.925
It is largely a loop road from the N16 linking Sligo and north County Leitrim. In Sligo, the road passes Sligo University Hospital on The Mall. Leaving Sligo, the road goes east via Hazelwood, St. Angela's College and Colgagh Lough before reaching the north shore of Lough Gill and entering County Leitrim. The road passes Parke's Castle before turning northeast to end at the N16. The R286 is long.

Geographic entities mentioned:
surface_form: Lough Gill
instance_of: Lake
countries: Ireland
coordinates: lat: 54.2542
lon: -8.38362
Pelvo di Ciabrera. The Pelvo di Ciabrera (3,152 m a.s.l.) is a mountain in the Cottian Alps, located on the main Alpine watershed between the Valle Varaita di Bellino and the Ubaye Valley. Characteristics. It lies on the border between France and Italy, between the communes of Bellino and Saint-Paul-sur-Ubaye. The main watershed ridge in this area has a general north-south trend from the to the.

Geographic entities mentioned:
surface_form: Ubaye Valley
instance_of: Valley
countries: France
coordinates: lat: 44.433780555556
lon: 6.6563416666667
surface_form: pelvo di ciabrera
instance_of: Mountain
countries: Italy
coordinates: lat: 44.5796
lon: 6.93329
Pelvo di Ciabrera. The Pelvo di Ciabrera (3,152 m a.s.l.) is a mountain in the Cottian Alps, located on the main Alpine watershed between the Valle Varaita di Bellino and the Ubaye Valley. Characteristics. It lies on the border between France and Italy, between the communes of Bellino and Saint-Paul-sur-Ubaye. The main watershed ridge in this area has a general north-south trend from the to the.

Geographic entities mentioned:
surface_form: pelvo di ciabrera
instance_of: Mountain
countries: Italy
coordinates: lat: 44.5796
lon: 6.93329
Tropheops microstoma. &quot;Tropheops microstoma&quot; is a species of cichlid fish endemic to Lake Malawi where it prefers sheltered bays with calm waters. This species can reach a length of SL. It can also be found in the aquarium trade.

Geographic entities mentioned:
surface_form: Lake Malawi
instance_of: Lake
countries: Malawi
Mozambique
Tanzania
coordinates: lat: -12.183333333333
lon: 34.366666666667
There are about forty islands and skerries. Only four are inhabited, and only nine are larger than. The largest and most populous are Arran and Bute. They are served by dedicated ferry routes, as are Great Cumbrae and Holy Island. Unlike the isles in the four larger Scottish archipelagos, none of the isles in this group are connected to one another or to the mainland by bridges.

Geographic entities mentioned:
surface_form: Holy Island
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 55.525
lon: -5.0722222222222
The Highland Boundary Fault runs past Bute and through the northern part of Arran. Therefore, from a geological perspective, some of the islands are in the Highlands and some in the Central Lowlands. As a result of Arran's geological similarity to Scotland, it is sometimes referred to as &quot;Scotland in miniature&quot; and the island is a popular destination for geologists.

Geographic entities mentioned:
surface_form: Central Lowlands
instance_of: Valley
countries: United Kingdom
coordinates: lat: 56.408
lon: -4.044
White fonio has its main growing region in the highland plateaus of Nigeria, where it is popularly called &quot;acha&quot;. The second fonio species, &quot;iburu&quot; or black fonio, is limited to the Jos-Bauchi Plateau in Nigeria and the northern regions of Togo and Benin. Fonio is grown in parts of the Dominican Republic, first only grown as a weed, but it is now cultivated again.

Geographic entities mentioned:
surface_form: Jos-Bauchi Plateau
instance_of: Plateau
countries: Nigeria
coordinates: lat: 9.5667
lon: 9.0833
Sasso di Bosconero. Sasso di Bosconero () (2,468 m) is the highest mountain of the &quot;Bosconero Range&quot;, a subgroup of the southern Dolomites in Veneto, Italy. It appears as a giant pyramid that hangs over the Zoldo Valley, near the town of Longarone. It was first climbed in 1878 by Cesare Tomè and Gottfried Merzbacher along with local guide Santo Siorpaes.

Geographic entities mentioned:
surface_form: sasso di bosconero
instance_of: Mountain
countries: Italy
coordinates: lat: 46.3375
lon: 12.2675
Huu-ay-aht First Nations. The Huu-ay-aht First Nations is a First Nations based on Pachena Bay about northwest of Victoria, British Columbia, on the west coast of Vancouver Island, in Canada. The traditional territories of the Huu-ay-aht make up the watershed of the Sarita River. The Huu-ay-aht is a member of the Nuu-chah-nulth Tribal Council and is a member of the Maa-nulth Treaty Society.

Geographic entities mentioned:
surface_form: Sarita River
instance_of: Watercourse
countries: Canada
coordinates: lat: 48.89802
lon: -125.00193
Under the name &quot;jota&quot;, it is typical and especially popular in Trieste and its province (where it is considered to be the prime example of Triestine food), in the Istrian peninsula, in the province of Gorizia, in the whole Slovenian Littoral, in the Rijeka area, and in Friuli, especially in some of its peripheral areas (the highland region of Carnia, the Torre and Natisone river valleys or Slavia Veneta).

Geographic entities mentioned:
surface_form: Carnia
instance_of: Valley
countries: Italy
coordinates: lat: 46.39444444
lon: 12.77416667
Climate. Gorizia has a humid subtropical climate (Köppen climate classification &quot;Cfa&quot;). The town is located at the confluence of the Isonzo and Vipava Valleys. It lies on a plain overlooked by the Gorizia Hills. Sheltered from the north and from the east by a mountain ridge, Gorizia is completely protected from the cold bora wind, which affects the rest of the neighboring areas.

Geographic entities mentioned:
surface_form: Vipava Valley
instance_of: Valley
countries: Slovenia
coordinates: lat: 45.876147222222
lon: 13.907319444444
A story on his adventures also appeared in the October 1959 issue of &quot;Outdoor Life&quot; magazine. In 1964, he canoed 300 miles from Great Slave Lake to the Mackenzie River delta. The Arctic Ocean was iced in by the time he arrived, and Dauksza was forced to walk to an Eskimo camp.

Geographic entities mentioned:
surface_form: Great Slave Lake
instance_of: Lake
countries: Canada
coordinates: lat: 61.666666666667
lon: -114
Oreochromis tanganicae. &quot;Oreochromis tanganicae&quot;, the Tanganyika tilapia, is a species of cichlid endemic to Lake Tanganyika and the mouths of its larger affluent rivers. This species can reach a length of SL. Males are larger and more colorful than females and possess longer dorsal and anal fins when fully grown. In the wild, the species is primarily herbivorous.

Geographic entities mentioned:
surface_form: Lake Tanganyika
instance_of: Lake
countries: Tanzania
Democratic Republic of the Congo
Burundi
Zambia
coordinates: lat: -6.1
lon: 29.5
Lake View Cemetery (Seattle). Lake View Cemetery is a private cemetery located in Seattle, Washington, in the Capitol Hill neighborhood, just north of Volunteer Park. Known as &quot;Seattle's Pioneer Cemetery,&quot; it is run by an independent, non-profit association. It was founded in 1872 as the Seattle Masonic Cemetery and later renamed for its view of Lake Washington to the east. Monuments.

Geographic entities mentioned:
surface_form: Lake Washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
Arleta High School. Arleta High School (AHS) is a secondary school located on Van Nuys Boulevard in the Arleta section of Los Angeles, California, United States in the San Fernando Valley. History. The school opened on October 3, 2006, serving grades 9 through 10 during its first year of operation. It is part of the Los Angeles Unified School District.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
Brebeneskul. Brebeneskul (,) is a peak in the Chornohora region of Ukraine, with a height of 2,035 meters above sea level. It is the second-highest peak in Ukraine.

Geographic entities mentioned:
surface_form: brebeneskul
instance_of: Mountain
countries: Ukraine
coordinates: lat: 48.0975
lon: 24.58
surface_form: brebeneskul
instance_of: Lake
countries: Ukraine
coordinates: lat: 48.101666666667
lon: 24.562277777778
It was established on January 25, 2001 to protect the headwaters of the Spatsizi River while providing recreational facilities for visitors. Geography. The park is located just east of Mount Gunanoot in the Skeena Mountains of north-central British Columbia. Here the river emerges out from the mountains to flow north through the park and on toward Spatsizi Plateau Wilderness Provincial Park.

Geographic entities mentioned:
surface_form: Mount Gunanoot
instance_of: Mountain
countries: Canada
coordinates: lat: 57.1114
lon: -128.894
Stone Lake (California). Stone Lake is in Stone Lake State Park, a California State Park, located in Sacramento County, California. The open space property protects two rare natural Central Valley lakes and their surrounding riparian habitat and grassland areas. The County of Sacramento operates Stone Lake.

Geographic entities mentioned:
surface_form: central valley
instance_of: Valley
countries: United States
coordinates: lat: 37.706111111111
lon: -120.99138888889
Stone Lake (California). Stone Lake is in Stone Lake State Park, a California State Park, located in Sacramento County, California. The open space property protects two rare natural Central Valley lakes and their surrounding riparian habitat and grassland areas. The County of Sacramento operates Stone Lake.

Geographic entities mentioned:
surface_form: stone lake
instance_of: Lake
countries: United States
coordinates: lat: 36.717
lon: -106.877
surface_form: stone lake (california)
instance_of: Landform
countries: United States
coordinates: lat: 38.3456
lon: -121.498
Stone Lake (California). Stone Lake is in Stone Lake State Park, a California State Park, located in Sacramento County, California. The open space property protects two rare natural Central Valley lakes and their surrounding riparian habitat and grassland areas. The County of Sacramento operates Stone Lake.

Geographic entities mentioned:
surface_form: stone lake
instance_of: Lake
countries: United States
coordinates: lat: 36.717
lon: -106.877
surface_form: stone lake
instance_of: Lake
countries: United States
coordinates: lat: 36.717
lon: -106.877
surface_form: stone lake
instance_of: Landform
countries: United States
coordinates: lat: 38.3456
lon: -121.498
surface_form: stone lake
instance_of: Landform
countries: United States
coordinates: lat: 38.3456
lon: -121.498
Stone Lake (California). Stone Lake is in Stone Lake State Park, a California State Park, located in Sacramento County, California. The open space property protects two rare natural Central Valley lakes and their surrounding riparian habitat and grassland areas. The County of Sacramento operates Stone Lake.

Geographic entities mentioned:
surface_form: stone lake
instance_of: Lake
countries: United States
coordinates: lat: 36.717
lon: -106.877
surface_form: stone lake
instance_of: Landform
countries: United States
coordinates: lat: 38.3456
lon: -121.498
Geographic range. &quot;F. erytrogramma&quot; is found from southern Maryland to southeastern Louisiana, including eastern Virginia, southeastern North Carolina, South Carolina, Georgia, northern Florida, Alabama and Mississippi. A small population once inhabited the Lake Okeechobee region of southern Florida, but was declared extinct on October 5, 2011.

Geographic entities mentioned:
surface_form: Lake Okeechobee
instance_of: Lake
countries: United States
coordinates: lat: 26.933333333333
lon: -80.8
The eruptions at the Chaos Crags mark one of just three instances of Holocene activity within the Lassen volcanic center. The cluster of domes is located north of Lassen Peak and form part of the southernmost segment of the Cascade Range in Northern California. Each year, a lake forms at the base of the Crags, and typically dries by the end of the summer season.

Geographic entities mentioned:
surface_form: Lassen Peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.488055555555555
lon: -121.505
From the base of the crags and extending toward the northwest corner of the park is Chaos Jumbles, a rock avalanche that undermined Chaos Crags' northwest slope 300 years ago. Riding on a cushion of compressed air (see sturzstrom), the rock debris traveled at about, flattened the forest before it, and dammed Manzanita Creek, forming Manzanita Lake.

Geographic entities mentioned:
surface_form: Manzanita Lake
instance_of: Lake
countries: United States
coordinates: lat: 40.533711111111
lon: -121.5678
Geography. The Chaos Crags form part of the southernmost segment of the Cascade Range in Northern California. They lie in the northwest corner of the Lassen Volcanic National Park, in Shasta County. Located to the north of Lassen Peak, they have an elevation of about. The Lassen Volcanic National Park area is surrounded by the Lassen National Forest, which has an area of.

Geographic entities mentioned:
surface_form: Lassen Peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.488055555555555
lon: -121.505
They lack a summit crater. The domes began forming about 1,100 years ago, beginning with vent-opening eruptions, then vigorous explosive eruptions of pumice and ash followed by effusive activity. This created unstable edifices that partially collapsed and formed pyroclastic flows, similar to the most recent eruptions at the Mono–Inyo Craters.

Geographic entities mentioned:
surface_form: Mono–Inyo Craters
instance_of: Mountain
countries: United States
coordinates: lat: 37.88333333
lon: -119
The rockslide moved at about, partly moving on a cushion of compressed air, which lowered friction. The formation of the Jumbles covered with volcanic blocks, causing the formation of Manzanita Lake by damming Manzanita Creek. The rockfall impeded soil development and tree growth in the Chaos Jumbles area, which has been slower than in the Devastated Area near Lassen Peak.

Geographic entities mentioned:
surface_form: Manzanita Lake
instance_of: Lake
countries: United States
coordinates: lat: 40.533711111111
lon: -121.5678
These eruptions formed the Lassen dome field, staged as andesite lava flows surrounding two sequences of dacitic lava domes. The first sequence of lava domes, known as the Bumpass domes, formed between 300,000 and 190,000 years ago, while the production of the younger Eagle Peak domes began about 70,000 years ago.

Geographic entities mentioned:
surface_form: eagle peak
instance_of: Mountain
countries: United States
coordinates: lat: 33.6769
lon: -108.577
All three sequences — Bumpass, Eagle Peak, and Twin Lakes — formed from lava subjected to magma-mixing processes, accounting for their heterogeneous appearance and composition. Because of these mixing mechanisms, lavas may have different compositions but similar appearances, or similar compositions with different appearances.

Geographic entities mentioned:
surface_form: eagle peak
instance_of: Mountain
countries: United States
coordinates: lat: 33.6769
lon: -108.577
surface_form: twin lakes
instance_of: Lake
countries: United States
coordinates: lat: 27.893888888889
lon: -81.594722222222
surface_form: twin lakes
instance_of: Lake
countries: United States
coordinates: lat: 43.4834018
lon: -74.9490486
The eruption that produced the Chaos Crags consisted of more than 90% mixed magma, and likely resulted from the interaction of felsic and mafic magmas. The Eagle Peak Sequence, which includes the Chaos Crags, consists of seven dacite and rhyodacite lava domes and lava flows, along with pyroclastic rock deposits.

Geographic entities mentioned:
surface_form: eagle peak
instance_of: Mountain
countries: United States
coordinates: lat: 33.6769
lon: -108.577
surface_form: chaos crags
instance_of: Mountain
countries: United States
coordinates: lat: 40.524166666667
lon: -121.52111111111
The Chaos Crags consist of five small lava domes, made of rhyodacite, which line up with the western edge of the Mount Tehama caldera. The youngest part of the Lassen volcanic center's dome field and the youngest domes in the Eagle Peak sequence, they reach an elevation of about above their surroundings. They lack a summit crater.

Geographic entities mentioned:
surface_form: eagle peak
instance_of: Mountain
countries: United States
coordinates: lat: 33.6769
lon: -108.577
surface_form: lassen volcanic center
instance_of: Mountain
countries: United States
coordinates: lat: 40.488055555555555
lon: -121.505
Other plants found in the area consist of coyote mint, lupines, mule's ears, ferns, corn lilies, red mountain heathers, pinemat manzanitas,
greenleaf manzanitas, bush chinquapins, catchflies, Fremont's butterweed, buckwheat, granite gilia, mountain pride, mariposa tulips, creambush, and a variety of chaparral shrubs.

Geographic entities mentioned:
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 33.4867
lon: -86.8064
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.3918
lon: -121.145
The cause remains uncertain, but might have been an earthquake. The largest rockslide moved up nearby Table Mountain, then deflected and moved west. The rockslide moved at about, partly moving on a cushion of compressed air, which lowered friction. The formation of the Jumbles covered with volcanic blocks, causing the formation of Manzanita Lake by damming Manzanita Creek.

Geographic entities mentioned:
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.59807864926865
lon: -121.55626585419016
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 35.9061
lon: -120.276
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.847774
lon: -121.713574
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.2958046
lon: -110.0553458
The first sequence of lava domes, known as the Bumpass domes, formed between 300,000 and 190,000 years ago, while the production of the younger Eagle Peak domes began about 70,000 years ago. The andesite lava flows form the older and younger Twin Lakes sequences, and date to between 315,000 and 240,000 years ago and between 90,000 years ago and present, respectively.

Geographic entities mentioned:
surface_form: twin lakes
instance_of: Lake
countries: United States
coordinates: lat: 27.893888888889
lon: -81.594722222222
surface_form: twin lakes
instance_of: Lake
countries: United States
coordinates: lat: 43.4834018
lon: -74.9490486
They formed as six dacite domes about 1,000 years ago, one dome collapsing during an explosive eruption about 70 years later. The eruptions at the Chaos Crags mark one of just three instances of Holocene activity within the Lassen volcanic center. The cluster of domes is located north of Lassen Peak and form part of the southernmost segment of the Cascade Range in Northern California.

Geographic entities mentioned:
surface_form: lassen volcanic center
instance_of: Mountain
countries: United States
coordinates: lat: 40.488055555555555
lon: -121.505
surface_form: chaos crags
instance_of: Mountain
countries: United States
coordinates: lat: 40.524166666667
lon: -121.52111111111
It usually dries up by the end of August. Geology. Between 385,000 and 315,000 years ago, volcanic activity in the Lassen volcanic center shifted dramatically from building andesitic stratovolcanoes to producing lava domes made of dacite. These eruptions formed the Lassen dome field, staged as andesite lava flows surrounding two sequences of dacitic lava domes.

Geographic entities mentioned:
surface_form: lassen volcanic center
instance_of: Mountain
countries: United States
coordinates: lat: 40.488055555555555
lon: -121.505
The andesite lava flows form the older and younger Twin Lakes sequences, and date to between 315,000 and 240,000 years ago and between 90,000 years ago and present, respectively. Beginning 190,000 years ago, eruptions ceased in the Lassen Volcanic center for 100,000 years.

Geographic entities mentioned:
surface_form: lassen volcanic center
instance_of: Mountain
countries: United States
coordinates: lat: 40.488055555555555
lon: -121.505
Of the five remaining domes, two have had landslides at their domes. The dome-forming eruptions at Chaos Crags, along with the eruption of Cinder Cone and the 1914–1921 eruptions of Lassen Peak, constitute the only Holocene activity within the Lassen volcanic center.

Geographic entities mentioned:
surface_form: lassen volcanic center
instance_of: Mountain
countries: United States
coordinates: lat: 40.488055555555555
lon: -121.505
surface_form: lassen peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.488055555555555
lon: -121.505
surface_form: chaos crags
instance_of: Mountain
countries: United States
coordinates: lat: 40.524166666667
lon: -121.52111111111
The Chaos Crags are monitored for movement in case of future rockslides by the United States Geological Survey; GPS receivers have been in place to monitor deformation within the Lassen volcanic center since 2008. Thirteen seismometers in the vicinity, first installed in 1976 and since updated each decade, continually survey earthquakes within the locale. Ecology.

Geographic entities mentioned:
surface_form: lassen volcanic center
instance_of: Mountain
countries: United States
coordinates: lat: 40.488055555555555
lon: -121.505
Domes B through F followed in that order, though their exact ages remain unclear. Lasting from 1,125 to 1,060 years ago, this eruptive phase resembled the Lassen Peak eruptions in May 1915, though the Chaos Crag eruption had a magnitude 100 times greater, with an output volume of.

Geographic entities mentioned:
surface_form: lassen peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.488055555555555
lon: -121.505
The Chaos Crags event may have been fed by the same reservoir of crystal-containing magma as the 25,000 BCE and 1914–1921 eruptions at Lassen Peak, based on shared zircon age spectra, composition, and phenocryst makeup, suggesting that they have all been fed by the same reservoir of crystal-containing magma.

Geographic entities mentioned:
surface_form: lassen peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.488055555555555
lon: -121.505
surface_form: chaos crags
instance_of: Mountain
countries: United States
coordinates: lat: 40.524166666667
lon: -121.52111111111
This magma chamber has recycled old magma cooling for many thousands of years, eventually heating the mixture so that it can be erupted. Unlike Lassen Peak, which has been altered by glaciers, the Chaos Crags have been unaffected by erosion. Their surfaces remain sharp with protrusions.

Geographic entities mentioned:
surface_form: lassen peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.488055555555555
lon: -121.505
surface_form: chaos crags
instance_of: Mountain
countries: United States
coordinates: lat: 40.524166666667
lon: -121.52111111111
The rockslide moved at about, partly moving on a cushion of compressed air, which lowered friction. The formation of the Jumbles covered with volcanic blocks, causing the formation of Manzanita Lake by damming Manzanita Creek. The rockfall impeded soil development and tree growth in the Chaos Jumbles area, which has been slower than in the Devastated Area near Lassen Peak.

Geographic entities mentioned:
surface_form: lassen peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.488055555555555
lon: -121.505
Thirteen seismometers in the vicinity, first installed in 1976 and since updated each decade, continually survey earthquakes within the locale. Ecology. Like the nearby Devastated Area by Lassen Peak, the Chaos Jumbles have skipped the usual plant regrowth phase dominated by herbaceous plants, moving directly to conifer regrowth. Crags Lake hosts tadpoles and many frogs.

Geographic entities mentioned:
surface_form: lassen peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.488055555555555
lon: -121.505
Chaos Crags. Chaos Crags is the youngest group of lava domes in Lassen Volcanic National Park, California. They formed as six dacite domes about 1,000 years ago, one dome collapsing during an explosive eruption about 70 years later. The eruptions at the Chaos Crags mark one of just three instances of Holocene activity within the Lassen volcanic center.

Geographic entities mentioned:
surface_form: chaos crags
instance_of: Mountain
countries: United States
coordinates: lat: 40.524166666667
lon: -121.52111111111
Each year, a lake forms at the base of the Crags, and typically dries by the end of the summer season. From the base of the crags and extending toward the northwest corner of the park is Chaos Jumbles, a rock avalanche that undermined Chaos Crags' northwest slope 300 years ago.

Geographic entities mentioned:
surface_form: chaos crags
instance_of: Mountain
countries: United States
coordinates: lat: 40.524166666667
lon: -121.52111111111
Riding on a cushion of compressed air (see sturzstrom), the rock debris traveled at about, flattened the forest before it, and dammed Manzanita Creek, forming Manzanita Lake. In addition to the possibility of forming additional lava domes, future activity at the Chaos Crags could pose hazards from pumice, pyroclastic flows, or rockfalls.

Geographic entities mentioned:
surface_form: chaos crags
instance_of: Mountain
countries: United States
coordinates: lat: 40.524166666667
lon: -121.52111111111
In addition to the possibility of forming additional lava domes, future activity at the Chaos Crags could pose hazards from pumice, pyroclastic flows, or rockfalls. Geological study of the Chaos Crags, which continues today, began in the late 1920s, when Howel Williams wrote about its pyroclastic rock deposits, rockfall avalanches, and eruptions.

Geographic entities mentioned:
surface_form: chaos crags
instance_of: Mountain
countries: United States
coordinates: lat: 40.524166666667
lon: -121.52111111111
The Crags and the surrounding area's lakes and forests support numerous plant and animal species. The area is not a popular destination for visitors, despite its accessibility. The Chaos Crags and Crags Lake Trail, which lasts about three hours round-trip, offers views of volcanic phenomena nearby, as well as the Hat Creek valley and the Thousand Lakes Wilderness. Geography.

Geographic entities mentioned:
surface_form: chaos crags
instance_of: Mountain
countries: United States
coordinates: lat: 40.524166666667
lon: -121.52111111111
The Chaos Crags and Crags Lake Trail, which lasts about three hours round-trip, offers views of volcanic phenomena nearby, as well as the Hat Creek valley and the Thousand Lakes Wilderness. Geography. The Chaos Crags form part of the southernmost segment of the Cascade Range in Northern California. They lie in the northwest corner of the Lassen Volcanic National Park, in Shasta County.

Geographic entities mentioned:
surface_form: chaos crags
instance_of: Mountain
countries: United States
coordinates: lat: 40.524166666667
lon: -121.52111111111
Because of these mixing mechanisms, lavas may have different compositions but similar appearances, or similar compositions with different appearances. The eruption that produced the Chaos Crags consisted of more than 90% mixed magma, and likely resulted from the interaction of felsic and mafic magmas.

Geographic entities mentioned:
surface_form: chaos crags
instance_of: Mountain
countries: United States
coordinates: lat: 40.524166666667
lon: -121.52111111111
The Eagle Peak Sequence, which includes the Chaos Crags, consists of seven dacite and rhyodacite lava domes and lava flows, along with pyroclastic rock deposits. The Chaos Crags consist of five small lava domes, made of rhyodacite, which line up with the western edge of the Mount Tehama caldera.

Geographic entities mentioned:
surface_form: chaos crags
instance_of: Mountain
countries: United States
coordinates: lat: 40.524166666667
lon: -121.52111111111
Unlike Lassen Peak, which has been altered by glaciers, the Chaos Crags have been unaffected by erosion. Their surfaces remain sharp with protrusions. Unlike the vesicular and aphyric pyroclastic rock at Glass Mountain and Little Glass Mountain, lava deposits from the Chaos Crags are porphyritic with average vesicularity values at about 30%. Most of these vesicles exhibit oval shapes.

Geographic entities mentioned:
surface_form: chaos crags
instance_of: Mountain
countries: United States
coordinates: lat: 40.524166666667
lon: -121.52111111111