Sarmila/GeoWiki-Features huggingface dataset:
Shortly thereafter, it receives Badger Creek and Sunshine Creek from the left and the North Fork of Johnson Creek from the right. Turning sharply, Johnson Creek flows swiftly northwest for about, entering Gresham and shortly thereafter passing the United States Geological Survey (USGS) gauge at Regner Road, from the mouth.

Geographic entities mentioned:
surface_form: johnson creek
instance_of: Watercourse
countries: United States
coordinates: lat: 45.4442
lon: -122.643
Just beyond the cemetery, it receives Butler Creek on the left, enters Portland at about from the mouth, and receives Kelley Creek on the left shortly thereafter. Mitchell Creek, a major tributary of Kelley Creek, enters Kelley Creek about south of Johnson Creek. Shortly thereafter, Johnson Creek passes the USGS gauge station at Sycamore, from the mouth, and flows under Cedar Crossing Bridge.

Geographic entities mentioned:
surface_form: johnson creek
instance_of: Watercourse
countries: United States
coordinates: lat: 45.4442
lon: -122.643
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. Johnson Creek passes under Interstate 205, and shortly thereafter begins to flow more swiftly again at Southeast 82nd Avenue, about from the mouth.

Geographic entities mentioned:
surface_form: johnson creek
instance_of: Watercourse
countries: United States
coordinates: lat: 45.4442
lon: -122.643
Johnson Creek passes under Interstate 205, and shortly thereafter begins to flow more swiftly again at Southeast 82nd Avenue, about from the mouth. It then makes its sixth and seventh county-border crossings, dipping briefly into Clackamas County and back north into Multnomah County, and then runs near the border between Portland and Milwaukie along Johnson Creek Boulevard for about.

Geographic entities mentioned:
surface_form: johnson creek
instance_of: Watercourse
countries: United States
coordinates: lat: 45.4442
lon: -122.643
At Southeast 21st Avenue, it receives Crystal Springs Creek, which enters on the right. This tributary, long, begins on the Reed College campus, flows under the Blue Bridge in Reed Canyon, through the Crystal Springs Rhododendron Garden, and generally south to Johnson Creek.

Geographic entities mentioned:
surface_form: johnson creek
instance_of: Watercourse
countries: United States
coordinates: lat: 45.4442
lon: -122.643
This tributary, long, begins on the Reed College campus, flows under the Blue Bridge in Reed Canyon, through the Crystal Springs Rhododendron Garden, and generally south to Johnson Creek. From its confluence with Crystal Springs Creek, Johnson Creek flows south about, crossing the county border for the eighth and final time.

Geographic entities mentioned:
surface_form: johnson creek
instance_of: Watercourse
countries: United States
coordinates: lat: 45.4442
lon: -122.643
After re-entering Clackamas County, it passes the USGS gauge station at Milwaukie, from the mouth. Shortly thereafter, Johnson Creek empties into the Willamette River above its confluence with the Columbia River, which in turn flows about another to the Pacific Ocean at Astoria. Geology and topography.

Geographic entities mentioned:
surface_form: johnson creek
instance_of: Watercourse
countries: United States
coordinates: lat: 45.4442
lon: -122.643
Underlying the sediments are substantial thicknesses of basalt lavas from the Columbia River Basalt Group. The lava, exposed mainly in the uplands, has been folded and faulted to form a series of sub-basins, including the Johnson Creek watershed. The watershed is a roughly rectangular area of about.

Geographic entities mentioned:
surface_form: johnson creek
instance_of: Watercourse
countries: United States
coordinates: lat: 45.4442
lon: -122.643
The Kelso Slope, a northwest-sloping dissected surface west of the canyon of the Sandy River, tilts down from about above sea level near Sandy to about above sea level east of Gresham. Formed by the ancestral Columbia and Willamette Rivers, the terraces north of Johnson Creek are generally underlain by permeable sand and gravel.

Geographic entities mentioned:
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: johnson creek
instance_of: Watercourse
countries: United States
coordinates: lat: 45.4442
lon: -122.643
19th-century maps also show numerous springs and small streams flowing into a wetland that covered an area of today's southeast Portland between Powell Boulevard (U.S. Route 26) and Johnson Creek, a distance of. Though most of the wetland complex has been filled in and built upon, remnants exist at the Crystal Springs Rhododendron Garden on Crystal Springs Creek.

Geographic entities mentioned:
surface_form: johnson creek
instance_of: Watercourse
countries: United States
coordinates: lat: 45.4442
lon: -122.643
These streams and most others in this area were diverted into the city sewer system and no longer appear on the surface. A Johnson Creek near Hoyt Arboretum on the west side of the Willamette River in Portland has no relationship to the Johnson Creek on the east side. Volunteer group.

Geographic entities mentioned:
surface_form: johnson creek
instance_of: Watercourse
countries: United States
coordinates: lat: 45.4442
lon: -122.643
Before settlers moved into the basin, it consisted mainly of upland and wetland forests in which Native Americans fished, hunted, and foraged. Evidence suggests that people lived in the northern Oregon Cascade Range as early as 10,000 years ago. 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.

Geographic entities mentioned:
surface_form: johnson creek
instance_of: Watercourse
countries: United States
coordinates: lat: 45.4442
lon: -122.643
When Lewis and Clark visited the area in 1806, the Clackamas tribe consisted of about 1,800 people living in 11 villages. Epidemics of smallpox, malaria, and measles reduced this population to 88 by 1851, and in 1855 the tribe signed a treaty surrendering its lands, including Johnson Creek.

Geographic entities mentioned:
surface_form: johnson creek
instance_of: Watercourse
countries: United States
coordinates: lat: 45.4442
lon: -122.643
Epidemics of smallpox, malaria, and measles reduced this population to 88 by 1851, and in 1855 the tribe signed a treaty surrendering its lands, including Johnson Creek. By the middle of the 19th century, the European American newcomers had begun to remove vegetation, build sawmills, fell trees, fill wetlands, and farm in the fertile soil along Johnson Creek.

Geographic entities mentioned:
surface_form: johnson creek
instance_of: Watercourse
countries: United States
coordinates: lat: 45.4442
lon: -122.643
The creek is named for one of these newcomers, William Johnson, who in 1846 settled in what later became the Lents neighborhood of Portland and operated a water-powered sawmill. In early 1848 Lot Whitcomb, who would later found Milwaukie, filed a donation land claim and built a sawmill near the confluence of Johnson Creek and the Willamette River.

Geographic entities mentioned:
surface_form: johnson creek
instance_of: Watercourse
countries: United States
coordinates: lat: 45.4442
lon: -122.643
In 1886, plans were made for train tracks along the creek. 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.

Geographic entities mentioned:
surface_form: johnson creek
instance_of: Watercourse
countries: United States
coordinates: lat: 45.4442
lon: -122.643
By the 1920s, housing began to replace creekside farms. In the 1960s, the Oregon state government and Multnomah County proposed construction of a freeway along the creek connecting the Sellwood Bridge to Interstate 205. Floods. By removing the original vegetation, rural and urban development of the Johnson Creek watershed induced more rapid storm runoff and destructive floods.

Geographic entities mentioned:
surface_form: johnson creek
instance_of: Watercourse
countries: United States
coordinates: lat: 45.4442
lon: -122.643
Although substantially altering the stream and its aquatic life, this channel failed to prevent overflows, the largest of which damaged 1,200 structures in 1964. Precipitation patterns in the Johnson Creek watershed have contributed to frequent high flows and floods along the creek, typically between November and February.

Geographic entities mentioned:
surface_form: johnson creek
instance_of: Watercourse
countries: United States
coordinates: lat: 45.4442
lon: -122.643
About falls from November through February and only about from June through September. 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.

Geographic entities mentioned:
surface_form: johnson creek
instance_of: Watercourse
countries: United States
coordinates: lat: 45.4442
lon: -122.643
The second-highest level, occurred in November 1996, followed by the Christmas flood of 1964 on December 22, when the creek reached at Sycamore. As of 2008, the USGS was monitoring Johnson Creek at Regner Road in Gresham, from the mouth, and at Milwaukie, from the mouth, as well as at Sycamore. It also had stream-monitor stations on Kelley Creek and Crystal Springs Creek.

Geographic entities mentioned:
surface_form: johnson creek
instance_of: Watercourse
countries: United States
coordinates: lat: 45.4442
lon: -122.643
The Sycamore station was the oldest, having begun operation in 1941. Proposals by agencies such as Metro, the regional government of the Portland metropolitan area, and the U.S. Army Corps of Engineers in the 1970s and 1980s to control Johnson Creek flooding were abandoned after groups of residents objected to every proposal.

Geographic entities mentioned:
surface_form: johnson creek
instance_of: Watercourse
countries: United States
coordinates: lat: 45.4442
lon: -122.643
Army Corps of Engineers in the 1970s and 1980s to control Johnson Creek flooding were abandoned after groups of residents objected to every proposal. In 1990, the City of Portland formed the Johnson Creek Corridor Committee from multiple agencies and citizen groups with varied interests related to the watershed.

Geographic entities mentioned:
surface_form: johnson creek
instance_of: Watercourse
countries: United States
coordinates: lat: 45.4442
lon: -122.643
In 1990, the City of Portland formed the Johnson Creek Corridor Committee from multiple agencies and citizen groups with varied interests related to the watershed. Led by the city's Bureau of Environmental Services, the combined groups in 2001 produced the Johnson Creek Restoration Plan to reduce flooding, improve water quality, and improve fish and wildlife habitat.

Geographic entities mentioned:
surface_form: johnson creek
instance_of: Watercourse
countries: United States
coordinates: lat: 45.4442
lon: -122.643
Through 2007, at least 75 site-specific restoration projects had been carried out in the Johnson Creek Watershed, ranging from the $1.2 million Brookside Project, a constructed wetland, to small riparian repair projects. Most involved voluntary citizen participation in all phases, including the long-term management and care of the sites.

Geographic entities mentioned:
surface_form: johnson creek
instance_of: Watercourse
countries: United States
coordinates: lat: 45.4442
lon: -122.643
Pollution. The Oregon Department of Environmental Quality (DEQ) rated Johnson Creek's water quality between 1986 and 1995 as &quot;very poor&quot;. Monitoring the creek from the mouth, it recorded very high concentrations of nitrates and high concentrations of phosphates. Fecal coliform bacteria, total solids, and biochemical oxygen demand also impaired water quality.

Geographic entities mentioned:
surface_form: johnson creek
instance_of: Watercourse
countries: United States
coordinates: lat: 45.4442
lon: -122.643
High temperatures cause problems for aquatic life throughout the watershed. The Oregon standard for maximum temperatures conducive to salmonid rearing in the Willamette Basin is, and data show that the mean maximum summertime temperatures in Johnson Creek exceed this standard. The maximum temperature that Coho salmon can survive for short periods is.

Geographic entities mentioned:
surface_form: johnson creek
instance_of: Watercourse
countries: United States
coordinates: lat: 45.4442
lon: -122.643
Studies conducted by DEQ, USGS, the City of Gresham, and other public agencies have identified DDT (dichloro-diphenyl-trichloroethane), dieldrin, polychlorinated biphenyls (PCB), chlordane, and polycyclic aromatic hydrocarbons (PAH) as carcinogenic pollutants of Johnson Creek.

Geographic entities mentioned:
surface_form: johnson creek
instance_of: Watercourse
countries: United States
coordinates: lat: 45.4442
lon: -122.643
Generally, metal concentrations increase downstream. Macroinvertebrates and fish. A study conducted in 1999 for the City of Portland by researchers from Portland State University found that Johnson Creek had marginal conditions for macroinvertebrates, an important source of food for fish and other aquatic life.

Geographic entities mentioned:
surface_form: johnson creek
instance_of: Watercourse
countries: United States
coordinates: lat: 45.4442
lon: -122.643
The study compared differences in these life forms and in water chemistry from two urban streams, Johnson Creek and Tryon Creek in southwest Portland, with two nearby rural streams and found that benthic communities in the urban streams were degraded compared to the regional reference creeks. Most fish species in Johnson Creek tolerate warm water and disturbed conditions.

Geographic entities mentioned:
surface_form: johnson creek
instance_of: Watercourse
countries: United States
coordinates: lat: 45.4442
lon: -122.643
surface_form: johnson creek
instance_of: Watercourse
countries: United States
coordinates: lat: 45.4442
lon: -122.643
New plantings include native shrubs and trees such as red-osier dogwood, elderberry, Indian plum, and willow. City parks adjacent to Johnson Creek have areas devoted to marsh with shrubs, cattails, and smartweed, forested wetland, riparian woodland, open meadow, and orchard trees. Parks. By 1960, use of the rail line along Johnson Creek had declined and passenger service was discontinued.

Geographic entities mentioned:
surface_form: johnson creek
instance_of: Watercourse
countries: United States
coordinates: lat: 45.4442
lon: -122.643
Keahole Point. Keāhole Point is the westernmost point of the island of Hawaiʻi. The Kona International Airport was moved here from directly north of the town of Kailua-Kona in 1970, when the previous smaller airstrip was converted into the Old Kona Airport State Recreation Area. The name comes from &quot;Ke āhole&quot; since the āhole fish (Kuhlia sandvicensis) was found nearby.

Geographic entities mentioned:
surface_form: keahole point
instance_of: Landform
countries: United States
coordinates: lat: 19.725
lon: -156.058
Lake Vanda. Lake Vanda is a lake in Wright Valley, Victoria Land, Ross Dependency, Antarctica. The lake is long and has a maximum depth of. On its shore, New Zealand maintained Vanda Station from 1968 to 1995. At depths of greater than approximately 50 meters, Lake Vanda is a hypersaline lake with a salinity more than ten times that of seawater and more than the salinity of the Dead Sea.

Geographic entities mentioned:
surface_form: Wright Valley
instance_of: Valley
coordinates: lat: -77.166666666667
lon: 161.83333333333
Quequechan River. The Quequechan River is a river in Fall River, Massachusetts, that flows in a northwesterly direction from the northwest corner of the South Watuppa Pond through the heart of the city of Fall River and into the end of the Taunton River at Mount Hope Bay at Heritage State Park/Battleship Cove.

Geographic entities mentioned:
surface_form: South Watuppa Pond
instance_of: Lake
countries: United States
coordinates: lat: 41.706666666667
lon: -71.106111111111
The mills also used water for various processes involved in the manufacture of textiles. Hot, and used water was later returned directly to the river. In the years following the Civil War, with both sides of the river, and both Watuppa Ponds entirely within Massachusetts, there would be a remarkable expansion of the cotton textile industry within Fall River.

Geographic entities mentioned:
surface_form: Watuppa Ponds
instance_of: Lake
countries: United States
coordinates: lat: 41.706666666667
lon: -71.106111111111
In 1875, the Fall River Railroad was built to provide a rail connection with New Bedford. The railroad passed through the &quot;Narrows&quot; located between the North and South Watuppa Ponds, and over the shallow &quot;mill pond&quot; to Watuppa Station located at Plymouth Avenue. By the 1880s the quality of the water in the Quequechan River became a problem.

Geographic entities mentioned:
surface_form: Watuppa Ponds
instance_of: Lake
countries: United States
coordinates: lat: 41.706666666667
lon: -71.106111111111
Lady Evelyn Lake. Lady Evelyn Lake is a lake on the Lady Evelyn River in Timiskaming District, Northeastern Ontario, Canada. The highly irregularly shaped lake consists of two parts, about equal in size, separated by the Obisaga Narrows. The southern part is within the Obabika River Provincial Park, directly east of the Lady Evelyn-Smoothwater Provincial Park.

Geographic entities mentioned:
surface_form: lady evelyn lake
instance_of: Lake
countries: Canada
coordinates: lat: 47.3667
lon: -80.1792
Water drawn from the Sacramento–San Joaquin River Delta is transported down the San Joaquin Valley via the California Aqueduct and pumped over the Tehachapi Mountains, where it splits into the East Branch – providing water for Riverside and San Bernardino and eastern Los Angeles Counties – and the West Branch, which supplies western Los Angeles and parts of Ventura County.

Geographic entities mentioned:
surface_form: San Joaquin Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.628888888889
lon: -120.185
The mostly underground, pre-stressed concrete pipe has walls nearly thick. Water from the Foothill Feeder is stored in the smaller Los Angeles Reservoir in the San Fernando Valley. The water continues south via the Sepulveda Feeder, which provides water to Los Angeles proper and other municipalities in south Los Angeles and Orange Counties.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
2300 BC. Later developments. The Azapa Phase of local cultural development (4,000-2,500 BP) was a transitional period between the end of the Chinchorro Phase and the start of the Alto Ramírez Phase. These developments took place in the Azapa Valley near the coast. Around 4,000 BP, the people of the Azapa Valley saw some cultural changes brought by immigrants from the Altiplano.

Geographic entities mentioned:
surface_form: Azapa Valley
instance_of: Valley
countries: Chile
coordinates: lat: -18.51722222
lon: -70.19194444
These developments took place in the Azapa Valley near the coast. Around 4,000 BP, the people of the Azapa Valley saw some cultural changes brought by immigrants from the Altiplano. These influences led to the adoption of agriculture c. 3,000 BP, as well as the introduction of ceramics. These later groups no longer mummified their dead.

Geographic entities mentioned:
surface_form: Altiplano
instance_of: Plateau
countries: Bolivia
Peru
Chile
Argentina
coordinates: lat: -16.00358
lon: -69.65332
The influence of the early Andean cultures in northern Chile has been studied by several archaeologists. Especially the influence from the Wankarani culture, and the early Pukara culture from the Lake Titicaca area may be relevant here. During a transitional phase, the Chinchorros may have coexisted with an emergent Andean Tradition along the coast.

Geographic entities mentioned:
surface_form: Lake Titicaca
instance_of: Lake
countries: Peru
Bolivia
coordinates: lat: -15.825
lon: -69.325
Talysarn. Tal-y-sarn () is a village in the slate quarrying Nantlle Valley in Gwynedd, Wales, next to Penygroes. It is part of the community of Llanllyfni and includes some of Llandwrog. The ward had a population of 1,930 at the 2011 census, the built-up area having a population of 1,086.

Geographic entities mentioned:
surface_form: Nantlle Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.025
lon: -4.2833333333333
Mount Kashimayari. is a peak in the Hida Mountains range of the Japanese Alps at 2889m, located in Kurobe and Tateyama, Toyama and Ōmachi, Nagano, central Honshu, Japan. It is part of Chūbu-Sangaku National Park and is the second highest peak of the Ushirotateyama mountain range. It is one of the 100 Famous Japanese Mountains.

Geographic entities mentioned:
surface_form: tateyama
instance_of: Mountain
countries: Japan
coordinates: lat: 36.575833333333
lon: 137.61972222222
Mount Kashimayari. is a peak in the Hida Mountains range of the Japanese Alps at 2889m, located in Kurobe and Tateyama, Toyama and Ōmachi, Nagano, central Honshu, Japan. It is part of Chūbu-Sangaku National Park and is the second highest peak of the Ushirotateyama mountain range. It is one of the 100 Famous Japanese Mountains.

Geographic entities mentioned:
surface_form: mount kashimayari
instance_of: Mountain
countries: Japan
coordinates: lat: 36.624444
lon: 137.746944
Museo nazionale della Valcamonica. The Museo nazionale della Valcamonica is an archaeological museum located in the town of Cividate Camuno (Province of Brescia), which has a collection of Roman-period finds from various excavations which took place mostly in the 17th century in Val Camonica. Organization of the Collection.

Geographic entities mentioned:
surface_form: Val Camonica
instance_of: Valley
countries: Italy
coordinates: lat: 46.0075
lon: 10.3475
Hermitage Castle. Hermitage Castle is a semi-ruined castle in the border region of Scotland. It stands in the remote valley of the Hermitage Water, part of Liddesdale in Roxburghshire. It is under the care of Historic Scotland. The castle has a reputation, both from its history and its appearance, as one of the most sinister and atmospheric castles in Scotland. Origins of the name.

Geographic entities mentioned:
surface_form: Liddesdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 55.2
lon: -2.75
On 6 March 1492 Patrick Hepburn, 1st Earl of Bothwell had a charter of the lands and lordship of Liddesdale, including The Hermitage Castle, etc., upon the resignation of the same by Archibald Douglas, Earl of Angus, the latter getting the lordship of Bothwell (but not the Earldom) which Patrick in turn had resigned for the exchange.

Geographic entities mentioned:
surface_form: Liddesdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 55.2
lon: -2.75
Distribution and habitat. This species is present in western North America from British Columbia and western Alberta in the north to Baja California and central New Mexico in the south. There is also a small isolated population on the peak of Cerro Potosí, elevation 3,700 metres (12,200 ft), in Nuevo León, northeast Mexico.

Geographic entities mentioned:
surface_form: Cerro Potosí
instance_of: Mountain
countries: Mexico
coordinates: lat: 24.871666666667
lon: -100.2325
Foyers, Highland. Foyers (, meaning &quot;shelving slope&quot;) is a village in the Highland council area of Scotland, lying on the east shore of Loch Ness. The village is situated on the B852, part of the Military Road built by General George Wade, northeast of Fort Augustus.

Geographic entities mentioned:
surface_form: Loch Ness
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.3
lon: -4.45
The two are separated by the two waterfalls known as the Falls of Foyers. Since the late 19th century, water courses near Foyers have been harnessed to provide hydroelectricity. The British Aluminium Company built its first hydro-powered aluminium smelter at Foyers in 1896—the first in the UK—and it operated until 1967, powered by water captured in Loch Mhòr.

Geographic entities mentioned:
surface_form: Loch Mhòr
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.246
lon: -4.418
Liechtenstein prospered, however, during the decades following, as its economy modernized with the advantage of low corporate tax rates which drew many companies to the country. In 1949, Liechtenstein ceded the Ellhorn mountain to Switzerland as a result of Swiss demands and threats to, among other things, end the customs union between the two countries.

Geographic entities mentioned:
surface_form: Ellhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 47.05243
lon: 9.4788
The sanctuary offers limited access to tourism activities such as trekking, guided safaris, and bird watching. Some of the popular spots in and around the sanctuary include Berijam Lake, silent valley view, and the pine forests. In 2017, a tree walk facility was proposed at the sanctuary to promote environmental education and allow visitors to learn about the sanctuary's flora in a guided setting.

Geographic entities mentioned:
surface_form: Berijam Lake
instance_of: Lake
countries: India
coordinates: lat: 10.183333333333
lon: 77.395555555556
Milliken rode however he did not feature in the results for the first four stages. Stage 5 was marked by torrential downpours of rain hail and sleet as the riders climbed Mount Buffalo and Milliken suffered a puncture and had to wait more than an hour for a spare wheel. It was reported that Milliken was almost frozen and he abandoned the race.

Geographic entities mentioned:
surface_form: Mount Buffalo
instance_of: Mountain
countries: Australia
coordinates: lat: -36.777
lon: 146.767
Murovdağ. The Murovdağ or Mrav (anglicized as Murovdagh,;) is the highest mountain range in the Lesser Caucasus. The range is about long, and Gamish Mountain is its highest peak at. It is made up mainly of Jurassic, Cretaceous and Paleogene rocks. The Murovdağ ridge or Mrav range extends north from Hinaldag Peak through Gamish (or Gomshasar) Mountain.

Geographic entities mentioned:
surface_form: murovdagh
instance_of: Mountain
countries: Azerbaijan
coordinates: lat: 40.27
lon: 46.32
surface_form: murovdağ
instance_of: Mountain
countries: Azerbaijan
coordinates: lat: 40.27
lon: 46.32
surface_form: mrav
instance_of: Mountain
countries: Azerbaijan
coordinates: lat: 40.27
lon: 46.32
Murovdağ. The Murovdağ or Mrav (anglicized as Murovdagh,;) is the highest mountain range in the Lesser Caucasus. The range is about long, and Gamish Mountain is its highest peak at. It is made up mainly of Jurassic, Cretaceous and Paleogene rocks. The Murovdağ ridge or Mrav range extends north from Hinaldag Peak through Gamish (or Gomshasar) Mountain.

Geographic entities mentioned:
surface_form: murovdağ
instance_of: Mountain
countries: Azerbaijan
coordinates: lat: 40.27
lon: 46.32
The range is about long, and Gamish Mountain is its highest peak at. It is made up mainly of Jurassic, Cretaceous and Paleogene rocks. The Murovdağ ridge or Mrav range extends north from Hinaldag Peak through Gamish (or Gomshasar) Mountain. Geographically, it is a continuation of the Sevan mountains to the west.

Geographic entities mentioned:
surface_form: murovdağ
instance_of: Mountain
countries: Azerbaijan
coordinates: lat: 40.27
lon: 46.32
surface_form: mrav
instance_of: Mountain
countries: Azerbaijan
coordinates: lat: 40.27
lon: 46.32
Geographically, it is a continuation of the Sevan mountains to the west. The northeastern slope features a group of scenic lakes, including Göygöl near the northern slope. The Karabakh Plateau extends from the south of Murovdağ/Mrav. Fir and spruce forests are spread as far southeast as the Murovdağ.

Geographic entities mentioned:
surface_form: murovdağ
instance_of: Mountain
countries: Azerbaijan
coordinates: lat: 40.27
lon: 46.32
surface_form: mrav
instance_of: Mountain
countries: Azerbaijan
coordinates: lat: 40.27
lon: 46.32
The northeastern slope features a group of scenic lakes, including Göygöl near the northern slope. The Karabakh Plateau extends from the south of Murovdağ/Mrav. Fir and spruce forests are spread as far southeast as the Murovdağ. The summer mountain pastures of Murovdağ/Mrav were traditionally used by Azerbaijani and Armenian shepherds. Name.

Geographic entities mentioned:
surface_form: murovdağ
instance_of: Mountain
countries: Azerbaijan
coordinates: lat: 40.27
lon: 46.32
The Karabakh Plateau extends from the south of Murovdağ/Mrav. Fir and spruce forests are spread as far southeast as the Murovdağ. The summer mountain pastures of Murovdağ/Mrav were traditionally used by Azerbaijani and Armenian shepherds. Name. According to Armenian linguist Hrachia Acharian, the name &quot;Mrav&quot; derives from the Armenian word and means. History.

Geographic entities mentioned:
surface_form: murovdağ
instance_of: Mountain
countries: Azerbaijan
coordinates: lat: 40.27
lon: 46.32
surface_form: mrav
instance_of: Mountain
countries: Azerbaijan
coordinates: lat: 40.27
lon: 46.32
The Karabakh Plateau extends from the south of Murovdağ/Mrav. Fir and spruce forests are spread as far southeast as the Murovdağ. The summer mountain pastures of Murovdağ/Mrav were traditionally used by Azerbaijani and Armenian shepherds. Name. According to Armenian linguist Hrachia Acharian, the name &quot;Mrav&quot; derives from the Armenian word and means. History.

Geographic entities mentioned:
surface_form: mrav
instance_of: Mountain
countries: Azerbaijan
coordinates: lat: 40.27
lon: 46.32
Its southern slopes ran through the Martakert region of Nagorno-Karabakh. In late 1993–early 1994, the ridge was the scene of the bloodiest battle of the First Nagorno-Karabakh War that ended in an Armenian victory. During the 2020 Nagorno-Karabakh war, the peak of Murovdag came under Azerbaijani control.

Geographic entities mentioned:
surface_form: murovdag
instance_of: Mountain
countries: Azerbaijan
coordinates: lat: 40.27
lon: 46.32
The Murovdağ ridge or Mrav range extends north from Hinaldag Peak through Gamish (or Gomshasar) Mountain. Geographically, it is a continuation of the Sevan mountains to the west. The northeastern slope features a group of scenic lakes, including Göygöl near the northern slope. The Karabakh Plateau extends from the south of Murovdağ/Mrav.

Geographic entities mentioned:
surface_form: göygöl
instance_of: Lake
countries: Azerbaijan
coordinates: lat: 40.409722222222
lon: 46.326666666667
It was built in 1835 by Salvio Pacheco, a Californio ranchero with vast lands in Contra Costa. History. In 1834, Salvio Pacheco was awarded the Rancho Monte del Diablo Mexican land grant, including what is now known as Concord and parts of Pleasant Hill. On June 24, 1835, he completed this two-story adobe, the first building to be erected in Diablo Valley.

Geographic entities mentioned:
surface_form: Diablo Valley
instance_of: Valley
countries: United States
coordinates: lat: 37.9419
lon: -122.0598
The film was produced by Leon F. Douglass's National Color Film Company in the Lake Lagunitas area of Marin County, California, and was made in the Douglass Natural Color process. Douglass was also a partner in the founding of the Victor Talking Machine Company. The film stars Ruth Roland and Albert Morrison, and has walk-on appearances by Mary Pickford and Douglas Fairbanks.

Geographic entities mentioned:
surface_form: Lake Lagunitas
instance_of: Lake
countries: United States
coordinates: lat: 37.9475
lon: -122.59611111111
Etymology. The townland name is an anglicisation of the Gaelic placename &quot;Rath Caolain&quot; which is usually given as 'Keelan’s Fort' but a more likely explanation is &quot;Rath Caolán&quot;, meaning 'The Fort of the Little Narrow Place', as the townland is squeezed between the Shannon–Erne Waterway on the east side and Slieve Rushen on the west side.

Geographic entities mentioned:
surface_form: Slieve Rushen
instance_of: Mountain
countries: United Kingdom
Ireland
coordinates: lat: 54.151925
lon: -7.6426416666667
Geography. It is bounded on the north by Gortawee townland, on the east by Annagh townland, on the south by Doon (Tomregan) townland and on the west by Mucklagh townland. Its chief geographical features are the Shannon-Erne Waterway which flows north along its eastern boundary and a foothill of Slieve Rushen mountain reaching to above sea-level.

Geographic entities mentioned:
surface_form: Slieve Rushen
instance_of: Mountain
countries: United Kingdom
Ireland
coordinates: lat: 54.151925
lon: -7.6426416666667
The geography of Annaclone is typical of much of the area around the Mourne Mountains with rolling drumlins and farmland. Nearby Corbet Lough is visited by anglers while the highest point of the parish, locally known as 'the Knock', has views of the Mourne Mountains towards the south and Slieve Croob towards the north east. History.

Geographic entities mentioned:
surface_form: Slieve Croob
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.340088888889
lon: -5.9736722222222
Later the village became a city through a 1871 charter. In the 1830s, a government surveyor named John Brink named both Geneva Lake and Lake Geneva in Wisconsin after Geneva, New York. Geneva, Nebraska, founded in 1871, is considered to have been named after the one in New York, rather than directly for the Swiss city. Geography.

Geographic entities mentioned:
surface_form: Geneva Lake
instance_of: Lake
countries: United States
coordinates: lat: 42.59
lon: -88.435
Geneva, Nebraska, founded in 1871, is considered to have been named after the one in New York, rather than directly for the Swiss city. Geography. The town is at the wide northern outlet of Seneca Lake, a lake that spans south to Watkins Glen. Geneva is in the Finger Lakes region, the largest wine-producing area in New York State. The Cayuga-Seneca Canal is part of the watershed of Keuka Lake.

Geographic entities mentioned:
surface_form: Finger Lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 42.666666666667
lon: -76.833333333333
Geneva is in the Finger Lakes region, the largest wine-producing area in New York State. The Cayuga-Seneca Canal is part of the watershed of Keuka Lake. It flows north through Geneva, connecting to the Erie Canal, which was completed in 1825, giving access for the region to the Great Lakes and midwestern markets for their produce, as well as to buy natural resource commodities.

Geographic entities mentioned:
surface_form: Keuka Lake
instance_of: Lake
countries: United States
coordinates: lat: 42.496388888889
lon: -77.146111111111
He commanded the 840th Bombardment Squadron when the group went to the Mediterranean Theater of Operations, in March 1944, and became group operations officer in January 1945. He participated in the campaigns of Rome-Arno, Po Valley, Rhineland, North Apennines, Central Europe, Northern France, Southern France, and Southern Europe. He flew 52 combat missions during his World War II service.

Geographic entities mentioned:
surface_form: Po Valley
instance_of: Valley
countries: Italy
coordinates: lat: 45.330277777778
lon: 9.7988888888889
Mistassibi River. The Mistassibi River is a river in central Quebec, Canada. It is long and has a drainage basin of. Its source is an area with unnamed lakes about east of Canso Bay of Lake Albanel, eastern neighbor of Lake Mistassini. The name &quot;Mistassibi&quot;, only in use since the late 19th century, comes from the Innu-aimun language, meaning &quot;large river&quot;.

Geographic entities mentioned:
surface_form: Lake Albanel
instance_of: Lake
countries: Canada
coordinates: lat: 51.0833
lon: -73.0833
surface_form: Lake Mistassini
instance_of: Lake
countries: Canada
coordinates: lat: 51.00194444444445
lon: -73.61666666666666
Pardubice. Pardubice (;) is a city in the Czech Republic. It has about 92,000 inhabitants. It is the capital city of the Pardubice Region and lies on the Elbe River. The historic centre is well preserved and is protected as an urban monument reservation. Pardubice is known as the centre of industry, which represents an oil refinery or an electronic equipment plant.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
Geography. Pardubice is located about east of Prague. The city lies at the confluence of the Elbe and Chrudimka rivers. There are several fishponds, artificial lakes and oxbow lakes of the Elbe in the municipal territory. Pardubice is located in a predominantly flat agricultural lansdscape in the East Elbe Table, in the eastern part of the Polabí lowland.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
Heathen Maiden. The Heathen Maiden () is a rock formation that resembles a human face. It can be seen in the northern face of Mount Prisojnik near Kranjska Gora, in the Julian Alps in northwestern Slovenia. It is associated with a legend about a chamois known as Goldenhorn and a nymph (&quot;vila&quot;) dwelling in the mountain. Legend.

Geographic entities mentioned:
surface_form: Prisojnik
instance_of: Mountain
countries: Slovenia
coordinates: lat: 46.426002777777775
lon: 13.769130555555556
This was part of a general policy by Robert of redistributing lands and titles to his extended kin. Niall, however, had been married previously to Alyse de Crawford, by whom he had at least two sons, Sir Colin Og Campbell of Lochawe and Dubhghall. In 1315, King Robert granted the baronies of Loch Awe and Ardscotnish to Cailean for the service of a 40-oared galley for 40 days per annum.

Geographic entities mentioned:
surface_form: Loch Awe
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.291475
lon: -5.231141
Chiquito Peak. Chiquito Peak is a summit in the Cuyamaca Mountains of San Diego County, California, United States. It located north of Interstate 8 and about west of Descanso.

Geographic entities mentioned:
surface_form: chiquito peak
instance_of: Mountain
countries: United States
coordinates: lat: 32.8512
lon: -116.645
Coleophora nutantella. &quot;Coleophora nutantella&quot; is a moth of the family Coleophoridae. It is found from Fennoscandia to Spain, Sicily and Greece and from France to the Baltic states, Poland, Slovakia, Hungary and Romania. It is also found in Asia Minor. The wingspan is 14–18 mm. Adults are on wing from May to July.

Geographic entities mentioned:
surface_form: Fennoscandia
instance_of: Landform
countries: Norway
Sweden
Finland
Russia
Russian Empire
Soviet Union
coordinates: lat: 63
lon: 17
Shashan Mountains. Shashan or Koh-e-Shashan (Urdu: شاشان) is one of the highest mountains of Balochistan located in Gresha, Khuzdar District.

Geographic entities mentioned:
surface_form: shashan mountains
instance_of: Mountain
countries: Pakistan
coordinates: lat: 27.53277778
lon: 66.03388889
Trøa. Trøa is a village in Selbu Municipality in Trøndelag county, Norway. It is located along the eastern end of the lake Selbusjøen, just north of the village of Innbygda, about north of the municipal center of Mebonden, and about south of the village of Tømra. The village has a population (2024) of 234 and a population density of.

Geographic entities mentioned:
surface_form: Selbusjøen
instance_of: Lake
countries: Norway
coordinates: lat: 63.2312
lon: 10.9484
Central heights. The principal structures in Tenerife, make the central highlands, with the Teide–Pico Viejo complex and the Las Cañadas areas as most prominent. It comprises a semi-caldera of about in area, originated by several geological processes explained under the &quot;Origin and formation&quot; section.

Geographic entities mentioned:
surface_form: Pico Viejo
instance_of: Mountain
countries: Spain
coordinates: lat: 28.263888888889
lon: -16.664722222222
A known formation called &quot;Los Azulejos&quot;, composed by green-tinted rocks were created by hydrothermal processes. South of La Caldera is Guajara Mountain, which has an elevation of, rising above Teide National Park. At the bottom, is an endorheic basin flanked with very fine sedimentary material which has been deposited from its volcanic processes, and is known as Llano de Ucanca.

Geographic entities mentioned:
surface_form: Guajara Mountain
instance_of: Mountain
countries: Spain
coordinates: lat: 28.21694444
lon: -16.61166667
In 1954, the whole area around it was declared a national park, with further expansion later on. In addition, in June 2007 it was recognised by UNESCO as a World Heritage site. To the west lies the volcano Pico Viejo (Old Peak). On one side of it, is the volcano Chahorra o Narices del Teide, where the last eruption occurred in the vicinity of Mount Teide in 1798.

Geographic entities mentioned:
surface_form: Pico Viejo
instance_of: Mountain
countries: Spain
coordinates: lat: 28.263888888889
lon: -16.664722222222
Mount Gala represents its highest elevation at. The most unusual landscape of this massif is found on its southern coast, where the Acantilados de Los Gigantes (&quot;Cliffs of the Giants&quot;) present vertical walls reaching heights of in some places. The Adeje massif (&quot;Macizo de Adeje&quot;) is situated on the southern tip of the island.

Geographic entities mentioned:
surface_form: Acantilados de Los Gigantes
instance_of: Mountain
countries: Spain
coordinates: lat: 28.296521
lon: -16.855774
This contact with the Great Lakes attracted Sinclair and he was able to change his commission to serve on the lakes. He started out commanding ships on Lake Ontario but, in 1764, he was moved to the upper Great Lakes where he served until 1767. In 1767, he was removed from active service at Fort Sinclair, which he had built in 1764 under orders from Colonel John Bradstreet.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
Lake Everard. Lake Everard is an endorheic salt lake in South Australia, Australia. The lake, along with Lake Gairdner and Lake Harris form Lake Gairdner National Park. The lakebed of Lake Everard is generally salt crust, however, parts of the lake is saline clay with no salt crust. The lake was named after William Everard.

Geographic entities mentioned:
surface_form: Lake Gairdner
instance_of: Lake
countries: Australia
coordinates: lat: -31.566666666667
lon: 136
surface_form: lake gairdner
instance_of: Lake
countries: Australia
coordinates: lat: -31.566666666667
lon: 136
surface_form: gairdner
instance_of: Lake
countries: Australia
coordinates: lat: -31.566666666667
lon: 136
surface_form: gairdner
instance_of: Lake
countries: Australia
coordinates: lat: -31.566666666667
lon: 136
surface_form: lake harris
instance_of: Lake
countries: Australia
coordinates: lat: -31.06941
lon: 135.24203
Lake Everard. Lake Everard is an endorheic salt lake in South Australia, Australia. The lake, along with Lake Gairdner and Lake Harris form Lake Gairdner National Park. The lakebed of Lake Everard is generally salt crust, however, parts of the lake is saline clay with no salt crust. The lake was named after William Everard.

Geographic entities mentioned:
surface_form: lake everard
instance_of: Lake
countries: Australia
coordinates: lat: -31.43643
lon: 135.08794
Formed in 1970 and dissolved in 2015, all conference members belonged to the Wisconsin Interscholastic Athletic Association. 1970-1999. The Olympian Conference was formed in 1970 by eight small- to medium-sized high schools in proximity to the Fox River Valley and Lake Winnebago in east central Wisconsin.

Geographic entities mentioned:
surface_form: Lake Winnebago
instance_of: Lake
countries: United States
coordinates: lat: 44.0169756
lon: -88.4095327
Originally a natural lake, it was enlarged by the tall Fish Lake Dam, which impounds the north fork of Little Butte Creek, in the Rogue River watershed. Geology. Fish Lake is located between two volcanoes: Mount McLoughlin to the north and Brown Mountain to the south. Two-thousand-year-old andesite lava flows erupted from Brown Mountain surround Fish Lake's southern shore. History.

Geographic entities mentioned:
surface_form: Mount McLoughlin
instance_of: Mountain
countries: United States
coordinates: lat: 42.444472222222
lon: -122.31561111111
History. Fish Lake was originally a small natural lake. In 1898, the Fish Lake Water Company was established to help irrigate the Rogue Valley. The company proposed to enlarge Fish Lake and nearby Fourmile Lake for added water storage. The temporary Fish Lake Dam was constructed between 1902 and 1908. In 1906, Fourmile Lake Dam was constructed.

Geographic entities mentioned:
surface_form: Rogue Valley
instance_of: Valley
countries: United States
coordinates: lat: 42.440122222222
lon: -122.92615277778
Triana worked as an engineer for the train line of Puerto Wilches, finished in 1883, the central northern highway and train tracks in Cúcuta and on irrigation projects in the Valley of Sogamoso as part of a study to dewater Lake Tota. From 1890 Triana was director of public works in Nariño and from 1917 manager of the Municipal Tramway of Bogotá.

Geographic entities mentioned:
surface_form: Lake Tota
instance_of: Lake
countries: Colombia
coordinates: lat: 5.55
lon: -72.916666666667
Triana was interested in the former inhabitants of the Altiplano Cundiboyacense where he was born and studied the history of the Muisca (also called &quot;Chibcha&quot;, as the language they speak) and in 1922 he published his mayor work &quot;La Civilización Chibcha&quot; Other works are &quot;El jeroglífico Chibcha&quot; and &quot;Las leyendas Chibchas&quot;.

Geographic entities mentioned:
surface_form: Altiplano Cundiboyacense
instance_of: Plateau
countries: Colombia
coordinates: lat: 5.532209
lon: -73.362877
John W. Geary's Second Division was sent to the southern end of the ridge near Little Round Top; Brig. Gen. John Buford's cavalry division formed a skirmish line in the fields between Cemetery Ridge and Seminary Ridge. The III Corps arrived about 8 p.m. and replaced Geary's division (which was sent to Culp's Hill); the II Corps arrived about 10:30 p.m. and camped immediately behind the III Corps.

Geographic entities mentioned:
surface_form: Seminary Ridge
instance_of: Landform
countries: United States
coordinates: lat: 39.2536
lon: -77.2536
Gen. Ambrose Wright's Confederate brigade temporarily captured the southern end of the Angle before being driven back to Seminary Ridge by the Philadelphia Brigade. The Confederate artillery bombardment preceding Pickett's Charge on July 3 battered Cemetery Ridge, and Union artillery on the ridge counter-fired to Seminary Ridge.

Geographic entities mentioned:
surface_form: Seminary Ridge
instance_of: Landform
countries: United States
coordinates: lat: 39.2536
lon: -77.2536
Course. The creek begins at Jack Lake and flows east, passes under Ontario Highway 60, and flows into the southwest side of Mew Lake. It exits the lake at the northwest, flows north under Highway 60, turns east, and reaches its mouth at the North Madawaska River, which flows via the Madawaska River and the Ottawa River to the Saint Lawrence River. Recreation.

Geographic entities mentioned:
surface_form: Mew Lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.576944444444
lon: -78.518055555556