Sarmila/GeoWiki-Features huggingface dataset:
These were under temporary licences for testing, which are regularly awarded. RTÉast Networks also broadcast test DVB-T with analogue TV and radio channels from the Clermont Carn transmitter in the Cooley Mountains, County Louth with some signal bleed into Northern Ireland.

Geographic entities mentioned:
surface_form: Clermont Carn
instance_of: Mountain
countries: Ireland
coordinates: lat: 54.080055555556
lon: -6.3215638888889
Inglewood Golf Club. Inglewood Golf Club is a private golf club in the northwest United States in Kenmore, Washington. Founded in 1919 and opened for play in July 1921, it is located at the north end of Lake Washington, northeast of Seattle. Inglewood was designed by A. Vernon &quot;Mac&quot; Macan, a leading golf course architect of the time.

Geographic entities mentioned:
surface_form: Lake Washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
Geography. The park is the site of a natural freshwater aquifer, where water comes through the surface through cracks in basalt lava flow from Te Tātua a Riukiuta. Prior to European settlement, the land was primarily a pūriri lava rock forest ecosystem, a now rare ecosystem consisting of plants growing in a minimal soil environment, growing amongst rock and leaf humus. Early history.

Geographic entities mentioned:
surface_form: Te Tātua a Riukiuta
instance_of: Mountain
countries: New Zealand
coordinates: lat: -36.902944
lon: 174.754583
The aquifer and wetland have the traditional Māori name &quot;Te Wai Ōrea&quot; to, which means 'the waters of eels'. A traditional Māori story involves Ruarangi, a chief of the supernatural Patupaiarehe people, escaping a siege on Mount Albert through lava tunnels and emerging at Te Wai Ōrea. Later history.

Geographic entities mentioned:
surface_form: Mount Albert
instance_of: Mountain
countries: New Zealand
coordinates: lat: -36.891306
lon: 174.720306
Whitewater sports. Afon Tryweryn joins the River Dee roughly half a mile downstream from Bala Lake. The reservoir now at the head of Afon Tryweryn was created in 1965, to provide water to Liverpool. At that time, the 67 inhabitants of the village of Capel Celyn were forcibly removed.

Geographic entities mentioned:
surface_form: Bala Lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 52.883333333333
lon: -3.6333333333333
The Crown (mountain). The Crown, also known as Huang Guan Shan and sometimes Crown Peak, is a mountain in the Karakoram mountain range in China. It is located in the Xinjiang Uyghur Autonomous Region of China. About 42 kilometers from Chogori Peak. Its summit has an elevation of and it is the highest peak in the Yengisogat subrange of the Karakoram.

Geographic entities mentioned:
surface_form: the crown
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 36.1083
lon: 76.2125
The Crown (mountain). The Crown, also known as Huang Guan Shan and sometimes Crown Peak, is a mountain in the Karakoram mountain range in China. It is located in the Xinjiang Uyghur Autonomous Region of China. About 42 kilometers from Chogori Peak. Its summit has an elevation of and it is the highest peak in the Yengisogat subrange of the Karakoram.

Geographic entities mentioned:
surface_form: the crown
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 36.1083
lon: 76.2125
surface_form: huang guan shan
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 36.1083
lon: 76.2125
surface_form: crown peak
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 36.1083
lon: 76.2125
Yarrow. The village was first settled by Mennonites in the late 1920s, following the draining of Sumas Lake and the reclamation of the former lake bed for agriculture. It is at the foot of the Skagit Range of the Cascade Mountains on the Vedder River, near the latter's confluence with the Fraser, which traverses the Lower Mainland, of British Columbia.

Geographic entities mentioned:
surface_form: Sumas Lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.07
lon: -122.09
The Lower Mainland Ecoregion is part of the Pacific Maritime Ecozone. The village of Yarrow lies between Vedder Mountain to the south and Sumas Mountain to the northwest. The climate is temperate with most of the precipitation falling in the winter months as rain. The summer is warm and relatively dry.

Geographic entities mentioned:
surface_form: Vedder Mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 49.0664
lon: -122.012
surface_form: Sumas Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.9118
lon: -122.222
The climate is temperate with most of the precipitation falling in the winter months as rain. The summer is warm and relatively dry. The fertile upper Fraser Valley supports the growth of many varieties of fruit, vegetables and herbs. Yarrow's economy is thus primarily agricultural and includes dairy farms and field crops (blueberries, corn, cole crops and hay).

Geographic entities mentioned:
surface_form: Fraser Valley
instance_of: Valley
countries: Canada
coordinates: lat: 49.108333333333
lon: -122.29166666667
It was also part of the rivalry between the Ispahbudhan family and the Mihran family. Background. In 642/643, the Muslim Arabs had conquered Media, and continued to penetrate into the Iranian plateau. In 651, Farrukhzad, the &quot;spahbed&quot; of Khorasan, and minister of Yazdegerd III, mutinied and left for Tabaristan.

Geographic entities mentioned:
surface_form: Iranian plateau
instance_of: Plateau
countries: Iran
coordinates: lat: 36.283333
lon: 59.05
Saint Ephraim Monastery, Nea Makri. The Saint Ephraim Monastery (Greek: &quot;Μονή Αγίου Εφραίμ&quot;) is a women's monastery located on Mount Amomon in Attica, Greece. It is situated in the Xilokeriza area, east of Mount Pentelicus.

Geographic entities mentioned:
surface_form: Mount Pentelicus
instance_of: Mountain
countries: Greece
coordinates: lat: 38.08144
lon: 23.8825
Tinemaha Reservoir. Tinemaha Reservoir is a reservoir created by a dam on the Owens River in the Owens Valley. It is located in Inyo County, eastern California. It is part of the Los Angeles Aqueduct system, operated by the Los Angeles Department of Water and Power. The 1938 western film &quot;Under Western Stars&quot; starring Roy Rogers was filmed here.

Geographic entities mentioned:
surface_form: Owens Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.8025
lon: -118.199722
Genghis Hills. The Genghis Hills () are hills rising to to the south of Fuchs Dome and west of Stephenson Bastion, in the Shackleton Range, Antarctica. They were photographed from the air by the U.S. Navy, 1967, and surveyed by the British Antarctic Survey (BAS), 1968–71. They were named by the UK Antarctic Place-Names Committee in 1971 after Graham K.

Geographic entities mentioned:
surface_form: Fuchs Dome
instance_of: Mountain
coordinates: lat: -80.6
lon: -27.8333
surface_form: Stephenson Bastion
instance_of: Mountain
coordinates: lat: -80.7667
lon: -27.2
In an operation undertaken on the night of April 29, 2002, Yarden Morag and Shlomo Dvir drove a vehicle with a trailer to East Jerusalem. They were initially stopped near the Beit Orot Yeshiva by Mount Scopus, because it was irregular for Jews with skullcaps to drive in Palestinian areas of East Jerusalem, at night.

Geographic entities mentioned:
surface_form: Mount Scopus
instance_of: Mountain
countries: Israel
coordinates: lat: 31.7925
lon: 35.244166666667
Mountains in the Presidential Range are named for U.S. presidents, with the tallest (Mount Washington) named for the first president, the second tallest (Mount Adams) for the second president, and so on. However, due to a surveying error, Mount Monroe, named after the fifth president, James Monroe, is actually taller than Mount Madison. There are many hiking trails on the mountain.

Geographic entities mentioned:
surface_form: Mount Monroe
instance_of: Mountain
countries: United States
coordinates: lat: 44.255561111111
lon: -71.3225
surface_form: mount madison
instance_of: Mountain
countries: United States
coordinates: lat: 44.328333333333
lon: -71.278333333333
It is named after the fourth U.S. President, James Madison. Mountains in the Presidential Range are named for U.S. presidents, with the tallest (Mount Washington) named for the first president, the second tallest (Mount Adams) for the second president, and so on. However, due to a surveying error, Mount Monroe, named after the fifth president, James Monroe, is actually taller than Mount Madison.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: mount washington
instance_of: Mountain
countries: United States
coordinates: lat: 47.5311964
lon: -123.2459807
surface_form: mount adams
instance_of: Mountain
countries: United States
coordinates: lat: 44.0867
lon: -74.0258
surface_form: mount adams
instance_of: Mountain
countries: United States
coordinates: lat: 38.0075
lon: -105.605
surface_form: mount washington
instance_of: Mountain
countries: United States
coordinates: lat: 42.1019
lon: -73.4325
surface_form: mount washington
instance_of: Mountain
countries: United States
coordinates: lat: 38.9149
lon: -114.309
surface_form: mount washington
instance_of: Mountain
countries: United States
coordinates: lat: 40.4271
lon: -80.0112
surface_form: mount washington
instance_of: Mountain
countries: United States
coordinates: lat: 44.270827777778
lon: -71.303483333333
surface_form: mount adams
instance_of: Mountain
countries: United States
coordinates: lat: 44.320555555556
lon: -71.291388888889
surface_form: mount washington
instance_of: Mountain
countries: United States
coordinates: lat: 44.3321
lon: -121.839
surface_form: mount washington
instance_of: Mountain
countries: United States
coordinates: lat: 47.4259
lon: -121.7
surface_form: adams
instance_of: Mountain
countries: United States
coordinates: lat: 46.202411111111
lon: -121.49089444444
surface_form: mount adams
instance_of: Mountain
countries: United States
coordinates: lat: 46.202411111111
lon: -121.49089444444
There are many hiking trails on the mountain. A stretch of the Appalachian Trail traverses just below its summit on the Osgood Trail. The Madison Spring Hut, maintained by the Appalachian Mountain Club, is nestled between Mount Madison and Mount Adams and provides rustic lodging in the summer. Reservations generally need to be made far in advance.

Geographic entities mentioned:
surface_form: mount adams
instance_of: Mountain
countries: United States
coordinates: lat: 44.0867
lon: -74.0258
surface_form: mount madison
instance_of: Mountain
countries: United States
coordinates: lat: 44.328333333333
lon: -71.278333333333
surface_form: mount adams
instance_of: Mountain
countries: United States
coordinates: lat: 38.0075
lon: -105.605
surface_form: mount adams
instance_of: Mountain
countries: United States
coordinates: lat: 44.320555555556
lon: -71.291388888889
surface_form: adams
instance_of: Mountain
countries: United States
coordinates: lat: 46.202411111111
lon: -121.49089444444
surface_form: mount adams
instance_of: Mountain
countries: United States
coordinates: lat: 46.202411111111
lon: -121.49089444444
Mount Madison. Mount Madison is a mountain in the Presidential Range of New Hampshire in the United States. It is named after the fourth U.S. President, James Madison. Mountains in the Presidential Range are named for U.S. presidents, with the tallest (Mount Washington) named for the first president, the second tallest (Mount Adams) for the second president, and so on.

Geographic entities mentioned:
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: mount madison
instance_of: Mountain
countries: United States
coordinates: lat: 44.328333333333
lon: -71.278333333333
Mount Madison. Mount Madison is a mountain in the Presidential Range of New Hampshire in the United States. It is named after the fourth U.S. President, James Madison. Mountains in the Presidential Range are named for U.S. presidents, with the tallest (Mount Washington) named for the first president, the second tallest (Mount Adams) for the second president, and so on.

Geographic entities mentioned:
surface_form: mount madison
instance_of: Mountain
countries: United States
coordinates: lat: 44.328333333333
lon: -71.278333333333
The Madison Spring Hut, maintained by the Appalachian Mountain Club, is nestled between Mount Madison and Mount Adams and provides rustic lodging in the summer. Reservations generally need to be made far in advance. Mount Madison is the northernmost peak in the Presidentials. Like most of the range, its summit is above treeline.

Geographic entities mentioned:
surface_form: mount madison
instance_of: Mountain
countries: United States
coordinates: lat: 44.328333333333
lon: -71.278333333333
Mount Madison is the northernmost peak in the Presidentials. Like most of the range, its summit is above treeline. Due to high winds and low temperatures, hypothermia is a danger even in the summer. Climate. There is no weather station at the summit, but this climate table contains interpolated data for an area around the summit. Mount Madison has a subarctic climate (Köppen &quot;Dfc&quot;).

Geographic entities mentioned:
surface_form: mount madison
instance_of: Mountain
countries: United States
coordinates: lat: 44.328333333333
lon: -71.278333333333
Description. The park has a variety of geologic formations, including tall rock spires or hoodoos and steep cliffs, as well as open fields. Scenic overlooks include views of Pikes Peak. Within the park is a geological point of interest, Seven Castles, and a botanical reserve for yucca plants. Paseo Drive runs through the park to the horse stables.

Geographic entities mentioned:
surface_form: Pikes Peak
instance_of: Mountain
countries: United States
coordinates: lat: 38.840555555556
lon: -105.04416666667
The name of the wife of Alalcomenes was Athenaïs, and that of his son, Glaucopus, both of which refer to the goddess Athena. In some accounts, Alalcomenes was said to be the first man who appeared by Lake Copais before even the Moon was. He sprang spontaneously from the earth (Gaia) rather than being created by Prometheus and thus one of the men of the so-called golden race, subjects of Cronus.

Geographic entities mentioned:
surface_form: Lake Copais
instance_of: Lake
countries: Greece
coordinates: lat: 38.45
lon: 23.05
Etoi Ki. Etoi Ki () is a summit in the Pima County, Arizona, United States. It is west of Kitt Peak National Observatory and northwest of the unincorporated community of Sells. It is rises adjacent to Arizona State Route 86 across the highway from Bird Nest Hill on the Tohono O'odham Indian Reservation, about west of Tucson and north of the Mexican border.

Geographic entities mentioned:
surface_form: kitt peak
instance_of: Mountain
countries: United States
coordinates: lat: 31.963966666667
lon: -111.59983611111
Etoi Ki. Etoi Ki () is a summit in the Pima County, Arizona, United States. It is west of Kitt Peak National Observatory and northwest of the unincorporated community of Sells. It is rises adjacent to Arizona State Route 86 across the highway from Bird Nest Hill on the Tohono O'odham Indian Reservation, about west of Tucson and north of the Mexican border.

Geographic entities mentioned:
surface_form: etoi ki
instance_of: Mountain
countries: United States
coordinates: lat: 31.96361111
lon: -111.94694444
Bucher Glacier. Bucher Glacier () is a small glacier draining the west slopes of Rudozem Heights and flowing to Bourgeois Fjord just north of Bottrill Head on the German Peninsula, Fallières Coast on the west side of Graham Land, Antarctica. It was named by the UK Antarctic Place-Names Committee in 1958 for Edwin Bucher, Swiss glaciologist and author of many publications on snow and avalanches.

Geographic entities mentioned:
surface_form: Rudozem Heights
instance_of: Mountain
coordinates: lat: -67.65
lon: -66.7
This tarictic species complex is widely kept in captivity, but due to the taxonomic reorganization it is unknown if these birds are of pure descent. This occurs in a few protected areas such as Mount Apo, Mount Kitanglad, Pasonanca Natural Park, Mount Kalatungan and Mount Malindang but actual protection from illegal logging, hunting, and poaching are lax.

Geographic entities mentioned:
surface_form: Mount Kitanglad
instance_of: Mountain
countries: Philippines
coordinates: lat: 8.1427777777778
lon: 124.9125
surface_form: Mount Malindang
instance_of: Mountain
countries: Philippines
coordinates: lat: 8.2175
lon: 123.63666666667
The Dowager Duchess died in a car accident near Dungannon, County Tyrone, on 3 May 1987, aged 74. She was returning to Ely Lodge, on the shore of Lough Erne. Her funeral was held at St Macartin's Cathedral, Enniskillen amid high security during The Troubles due to her Royal, family connections and her son Gerald also being at the time the UK's richest man.

Geographic entities mentioned:
surface_form: Lough Erne
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.48262
lon: -7.80622
History. The Cline Buttes were named in honor of Doctor Cass A. Cline (1850–1926), a pioneer dentist and early land developer in central Oregon. A nearby waterfall on the Deschutes River, northeast of the buttes, is also named after the dentist. Cline immigrated to Oregon in 1853, settling in the Willamette Valley. He moved to central Oregon in 1871.

Geographic entities mentioned:
surface_form: Willamette Valley
instance_of: Valley
countries: United States
coordinates: lat: 44.9
lon: -123.1
From the summit of the Cline Buttes, visitors have an excellent view of Cascade peaks to the west as well as the high desert country of Deschutes and Crook counties to the east. Visitors can see as far north as Mount Hood and as far south as Mount Bachelor from the Cline Buttes' highest summit. To the west are the central peaks of the Cascade Range, dominated by the Three Sisters.

Geographic entities mentioned:
surface_form: Mount Hood
instance_of: Mountain
countries: United States
coordinates: lat: 45.37361111111111
lon: -121.69583333333334
surface_form: Mount Bachelor
instance_of: Mountain
countries: United States
coordinates: lat: 43.979166666667
lon: -121.68833333333
surface_form: cline buttes
instance_of: Landform
countries: United States
coordinates: lat: 44.2529
lon: -121.30365
surface_form: bachelor
instance_of: Mountain
countries: United States
coordinates: lat: 43.979166666667
lon: -121.68833333333
Visitors can see as far north as Mount Hood and as far south as Mount Bachelor from the Cline Buttes' highest summit. To the west are the central peaks of the Cascade Range, dominated by the Three Sisters. To the northeast lies Smith Rock State Park, and farther to the east are the Powell Buttes and the Ochoco Mountains.

Geographic entities mentioned:
surface_form: Powell Buttes
instance_of: Mountain
countries: United States
coordinates: lat: 44.1797
lon: -120.9989
To the northeast lies Smith Rock State Park, and farther to the east are the Powell Buttes and the Ochoco Mountains. From the summit, the views to the south and southeast are of the lower sections of the Cline Buttes Recreation Area located on the Matson Plateau west of the Deschutes River with Pilot Butte and Paulina Peak in the distance.

Geographic entities mentioned:
surface_form: Paulina Peak
instance_of: Mountain
countries: United States
coordinates: lat: 43.68916667
lon: -121.255
surface_form: cline buttes
instance_of: Landform
countries: United States
coordinates: lat: 44.2529
lon: -121.30365
Cline Buttes. The Cline Buttes are mountains with volcanic origins that form three dome-shaped peaks located in Deschutes County in central Oregon. They are some of the eastern foothills of the Cascade Range. Situated on land administered by the Bureau of Land Management, the buttes are flanked on the east and west sides by two separate sections of the Eagle Crest Resort.

Geographic entities mentioned:
surface_form: cline buttes
instance_of: Landform
countries: United States
coordinates: lat: 44.2529
lon: -121.30365
The mountains have several hiking trails as well as a number of popular mountain bike routes. Geography and geology. The Cline Buttes are composed of three rounded peaks. They are some of the easternmost foothills of the Cascade mountain range, located near the northwest corner of Oregon's high desert country. The mountains are in Deschutes County, approximately west of Redmond.

Geographic entities mentioned:
surface_form: cline buttes
instance_of: Landform
countries: United States
coordinates: lat: 44.2529
lon: -121.30365
The mountains are in Deschutes County, approximately west of Redmond. Of the three crests, the southern peak is the highest. Its summit is above sea level. The Cline Buttes are a stand-alone mountain with the nearest higher peak to the south. Cline Buttes feature gentle slopes with highly conical shaped peaks.

Geographic entities mentioned:
surface_form: cline buttes
instance_of: Landform
countries: United States
coordinates: lat: 44.2529
lon: -121.30365
Its summit is above sea level. The Cline Buttes are a stand-alone mountain with the nearest higher peak to the south. Cline Buttes feature gentle slopes with highly conical shaped peaks. The Cline Buttes form a silicic volcanic center, active before the emplacement of the Deschutes Formation, a late Miocene to early Pliocene volcanic lava flow deposited between 7.5 and 5.3 million years ago.

Geographic entities mentioned:
surface_form: cline buttes
instance_of: Landform
countries: United States
coordinates: lat: 44.2529
lon: -121.30365
There are also some obsidian flow-bands exposed in a rock quarry on the northeast flank of the mountains. The Cline Buttes have been significantly eroded over time, leaving a rounded dome shape with three separate crests. They are now covered with of sandy loam soil in most areas with rhyolite and basalt outcropping on the steeper slopes.

Geographic entities mentioned:
surface_form: cline buttes
instance_of: Landform
countries: United States
coordinates: lat: 44.2529
lon: -121.30365
They are now covered with of sandy loam soil in most areas with rhyolite and basalt outcropping on the steeper slopes. The rhyolite lava flow deposits at Cline Buttes show a roughly porphyritic texture, with oligoclase phenocrysts making up between 1 and 2 percent of the minerals. These flows have been devitrified and show a normal-polarity magnetization.

Geographic entities mentioned:
surface_form: cline buttes
instance_of: Landform
countries: United States
coordinates: lat: 44.2529
lon: -121.30365
The rhyolite lava flow deposits at Cline Buttes show a roughly porphyritic texture, with oligoclase phenocrysts making up between 1 and 2 percent of the minerals. These flows have been devitrified and show a normal-polarity magnetization. Cline Buttes volcanoes also produced rhyodacite, which varies in color from light gray to red-brown and are similarly sparsely porphyritic.

Geographic entities mentioned:
surface_form: cline buttes
instance_of: Landform
countries: United States
coordinates: lat: 44.2529
lon: -121.30365
Environment and ecology. To the west of the Cline Buttes are woodlands covered with western juniper transitioning to ponderosa pine, lodgepole pine, and fir forest. The forest extends to the timberline on the central Cascade peaks, approximately away. The area south and east of the mountain is drier. It is typical of Oregon's high desert country dominated by juniper and sagebrush.

Geographic entities mentioned:
surface_form: cline buttes
instance_of: Landform
countries: United States
coordinates: lat: 44.2529
lon: -121.30365
The area south and east of the mountain is drier. It is typical of Oregon's high desert country dominated by juniper and sagebrush. The slopes of the Cline Buttes are covered by an old-growth juniper forest with an understory dominated by low sagebrush. Rabbitbrush is also a common understory shrub on the slopes.

Geographic entities mentioned:
surface_form: cline buttes
instance_of: Landform
countries: United States
coordinates: lat: 44.2529
lon: -121.30365
Rabbitbrush is also a common understory shrub on the slopes. Low groundcover plants includes Granite Gilia, rough eyelash, Longleaf hawksbeard, and bunch grass. The Cline Buttes and the surrounding area host a wide variety of wildlife. Larger mammals found in the area include black-tailed deer, elk, coyotes, black bear, bobcats, and cougars.

Geographic entities mentioned:
surface_form: cline buttes
instance_of: Landform
countries: United States
coordinates: lat: 44.2529
lon: -121.30365
Birds common to the Cline Buttes area include mountain chickadee, American goldfinch, lesser goldfinch, Black-headed grosbeak, mountain bluebird, Steller's jay, northern flickers, and black-billed magpie. Birds of prey found in the area include golden eagles, red-tailed hawks, northern harriers, and prairie falcons.

Geographic entities mentioned:
surface_form: cline buttes
instance_of: Landform
countries: United States
coordinates: lat: 44.2529
lon: -121.30365
Birds of prey found in the area include golden eagles, red-tailed hawks, northern harriers, and prairie falcons. While prairie falcons are uncommon in most parts of central Oregon, the area around the Cline Buttes has a native breeding population. To protect these birds, some areas around the Cline Buttes are closed to humans activities several months each year. History.

Geographic entities mentioned:
surface_form: cline buttes
instance_of: Landform
countries: United States
coordinates: lat: 44.2529
lon: -121.30365
To protect these birds, some areas around the Cline Buttes are closed to humans activities several months each year. History. The Cline Buttes were named in honor of Doctor Cass A. Cline (1850–1926), a pioneer dentist and early land developer in central Oregon. A nearby waterfall on the Deschutes River, northeast of the buttes, is also named after the dentist.

Geographic entities mentioned:
surface_form: cline buttes
instance_of: Landform
countries: United States
coordinates: lat: 44.2529
lon: -121.30365
In 1886, he filed a homestead land claim along the Deschutes River, near the buttes and falls that now bear his name. Later, Cline attempted to establish a town along the west bank of the Deschutes River, near the foot of the Cline Buttes. At its peak, the town of Cline Falls had a post office, a school, two stores, two hotels, a newspaper, a power plant, and 500 residential lots for sale.

Geographic entities mentioned:
surface_form: cline buttes
instance_of: Landform
countries: United States
coordinates: lat: 44.2529
lon: -121.30365
However, the community eventually failed when the first railroad route through the area was built on the opposite side of the river, through the neighboring town of Redmond. In 1904, gold was discovered on the Cline Buttes by Otto Retzlaff and C. P. Becker. The first gold ore was found in a ledge outcrop on the south flank of the mountain. More than 50 mining claims were quickly filed.

Geographic entities mentioned:
surface_form: cline buttes
instance_of: Landform
countries: United States
coordinates: lat: 44.2529
lon: -121.30365
More than 50 mining claims were quickly filed. However, when the ore was assayed it was found to be uneconomical to extract, so mining operations never got underway. In 1985, development of Eagle Crest Resort began along the Deschutes River, east of the Cline Buttes. The original development was on the east side of the Cline Falls Highway.

Geographic entities mentioned:
surface_form: cline buttes
instance_of: Landform
countries: United States
coordinates: lat: 44.2529
lon: -121.30365
In 1985, development of Eagle Crest Resort began along the Deschutes River, east of the Cline Buttes. The original development was on the east side of the Cline Falls Highway. In 1996, Eagle Crest began selling residential lots west of the Cline Falls Highway, between the highway and the eastern base of the Cline Buttes. This development was completed in 1993.

Geographic entities mentioned:
surface_form: cline buttes
instance_of: Landform
countries: United States
coordinates: lat: 44.2529
lon: -121.30365
This development was completed in 1993. Later, a third phase of Eagle Crest housing was developed along the northwestern base of the Cline Buttes. This area is separated from the Eagle Crest's second development by approximately one mile of Bureau of Land Management property. There is a paved easement road that connects the two areas, running along the northern base of the mountain.

Geographic entities mentioned:
surface_form: cline buttes
instance_of: Landform
countries: United States
coordinates: lat: 44.2529
lon: -121.30365
There is a paved easement road that connects the two areas, running along the northern base of the mountain. Today, the Bureau of Land Management administers the Cline Buttes and much of the land around the mountain. The bureau has established Cline Buttes Recreation Area, a area that is being developed for a wide range of recreational uses.

Geographic entities mentioned:
surface_form: cline buttes
instance_of: Landform
countries: United States
coordinates: lat: 44.2529
lon: -121.30365
Today, the Bureau of Land Management administers the Cline Buttes and much of the land around the mountain. The bureau has established Cline Buttes Recreation Area, a area that is being developed for a wide range of recreational uses. A service road runs up the south side of the mountain and then along the upper west flank to the main summit.

Geographic entities mentioned:
surface_form: cline buttes
instance_of: Landform
countries: United States
coordinates: lat: 44.2529
lon: -121.30365
There is also a road running along the east flank of the mountain. It leads to a rock quarry located on the northeast side of the mountain. Recreation. In the summer, recreation opportunities in the Cline Buttes area include hiking, horseback riding, mountain biking, bird watching, and scenic viewing. There are separate mountain trails for hikers, mountain bikes, and horseback riding.

Geographic entities mentioned:
surface_form: cline buttes
instance_of: Landform
countries: United States
coordinates: lat: 44.2529
lon: -121.30365
During the winter, the area is usually available for some recreation activities since snow accumulation on and around the mountain is not excessive in most years. The Cline Buttes are particularly well known for their mountain bike trails. Several of the bike trails are narrow single-track paths that follow the slope around the buttes to vista points.

Geographic entities mentioned:
surface_form: cline buttes
instance_of: Landform
countries: United States
coordinates: lat: 44.2529
lon: -121.30365
Those trails are recommended for expert bikers only. Many of the lower trails are narrow with occasional downhill jumps, suitable for bikers with intermediate-level skills. From the summit of the Cline Buttes, visitors have an excellent view of Cascade peaks to the west as well as the high desert country of Deschutes and Crook counties to the east.

Geographic entities mentioned:
surface_form: cline buttes
instance_of: Landform
countries: United States
coordinates: lat: 44.2529
lon: -121.30365
Geography and geology. The Cline Buttes are composed of three rounded peaks. They are some of the easternmost foothills of the Cascade mountain range, located near the northwest corner of Oregon's high desert country. The mountains are in Deschutes County, approximately west of Redmond. Of the three crests, the southern peak is the highest. Its summit is above sea level.

Geographic entities mentioned:
surface_form: cascade mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.307
lon: -111.588
surface_form: cascade mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.218611111111
lon: -73.860555555556
Van Gogh called his use of bright colors &quot;gymnastics&quot; that through experimentation created great depth, harmony and balance in his work. The painting contains a background of van Gogh's Japanese prints that were sold at Tanguy's shop. On top of Tanguy's hat is Mount Fuji; Kabuki actors share the wall with cherry trees in bloom.

Geographic entities mentioned:
surface_form: Mount Fuji
instance_of: Mountain
countries: Japan
coordinates: lat: 35.36055555555556
lon: 138.7275
History. Airport construction began in 1929 by orders of Huey Long, on a man-made peninsula dredged by the Orleans Levee Board, jutting into Lake Pontchartrain on the Eastern New Orleans side of the Industrial Canal. It was designed by New Orleans architect Leon C. Weiss and his firm Weiss, Dreyfous, and Seiferth, which also designed the Louisiana State Capitol.

Geographic entities mentioned:
surface_form: Lake Pontchartrain
instance_of: Lake
countries: United States
coordinates: lat: 30.188888888889
lon: -90.101388888889
Ammunition manufacturer Joyce Hornady was killed in a Piper Aztec on January 15, 1981. The aircraft, with Hornady at the controls flying in heavy fog, crashed into Lake Pontchartrain while on final approach to Lakefront Airport. Lakefront Airport was badly damaged by storm surge during Hurricane Katrina in 2005, and again during Hurricane Isaac in 2012.

Geographic entities mentioned:
surface_form: Lake Pontchartrain
instance_of: Lake
countries: United States
coordinates: lat: 30.188888888889
lon: -90.101388888889
Bennett Dome. Bennett Dome () is a rounded snow-covered peninsula on the south side of Beethoven Peninsula, Alexander Island, Antarctica. rising to about between Weber Inlet and Boccherini Inlet. It was photographed from the air by the Ronne Antarctic Research Expedition in 1947 and roughly mapped from the photographs by D. Searle of the Falkland Islands Dependencies Survey in 1960.

Geographic entities mentioned:
surface_form: bennett dome
instance_of: Mountain
coordinates: lat: -71.8
lon: -73.05
Bennett Dome. Bennett Dome () is a rounded snow-covered peninsula on the south side of Beethoven Peninsula, Alexander Island, Antarctica. rising to about between Weber Inlet and Boccherini Inlet. It was photographed from the air by the Ronne Antarctic Research Expedition in 1947 and roughly mapped from the photographs by D. Searle of the Falkland Islands Dependencies Survey in 1960.

Geographic entities mentioned:
surface_form: bennett dome
instance_of: Mountain
coordinates: lat: -71.8
lon: -73.05
surface_form: alexander
instance_of: Mountain
coordinates: lat: -63.3039
lon: -55.80564
Navy aerial photographs taken 1967–68 and from Landsat imagery taken 1972–73, and named by the Advisory Committee on Antarctic Names for Joseph E. Bennett, the head of the Polar Coordination and Information Section, Division of Polar Programs, National Science Foundation, 1976–86. Bennett Dome is one of the eight peninsulas of Alexander Island.

Geographic entities mentioned:
surface_form: bennett dome
instance_of: Mountain
coordinates: lat: -71.8
lon: -73.05
surface_form: alexander
instance_of: Mountain
coordinates: lat: -63.3039
lon: -55.80564
Bennett Dome. Bennett Dome () is a rounded snow-covered peninsula on the south side of Beethoven Peninsula, Alexander Island, Antarctica. rising to about between Weber Inlet and Boccherini Inlet. It was photographed from the air by the Ronne Antarctic Research Expedition in 1947 and roughly mapped from the photographs by D. Searle of the Falkland Islands Dependencies Survey in 1960.

Geographic entities mentioned:
surface_form: searle
instance_of: Mountain
coordinates: lat: -67.81666667
lon: -67.25
Cayuga Inlet. Cayuga Inlet is a river located in Tompkins County, New York. It flows into the south end of Cayuga Lake by Ithaca, New York. Development. Cayuga Inlet is a popular and well-connected location for boating.

Geographic entities mentioned:
surface_form: Cayuga Lake
instance_of: Lake
countries: United States
coordinates: lat: 42.68805555555556
lon: -76.70222222222222
Nietjärvi is a village by Lake Nietjärvi (&quot;järvi&quot; meaning lake). It is located in Ladoga Karelia, north of Lake Ladoga (in the southwestern corner of the Aunus Karelia frontier), in an area which belonged to Finland up to the end of the Continuation War (1944). Here, Finland's Aunus Group was on 11–12 July 1944 ready in positions at the defensive U-line, expecting an enemy offensive.

Geographic entities mentioned:
surface_form: Lake Ladoga
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 60.842777777777776
lon: 31.459722222222222
Until July 1944, the frontline had closely followed the banks of the River Svir, which flows from Lake Onega to Lake Ladoga. Before the battles began, the Finns abandoned the bridgehead which they had occupied on the southern shore of Svir, when troop transfers to the Karelian Isthmus made it impractical to hold.

Geographic entities mentioned:
surface_form: Lake Onega
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 61.690555555556
lon: 35.655555555556
surface_form: Lake Ladoga
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 60.842777777777776
lon: 31.459722222222222
The Finnish defense had prevented the Red Army from advancing from the north side of Lake Ladoga into the battle stages of the Karelian Isthmus. If the Red Army had not been stopped here, the Finnish forces fighting on the Karelian Isthmus would have been left between two Soviet armies on the narrow Isthmus, in the area limited by the Gulf of Finland in the south, and Lake Ladoga in the north.

Geographic entities mentioned:
surface_form: Lake Ladoga
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 60.842777777777776
lon: 31.459722222222222
In 1904 it again became property of the Congo Free State. In 1908, it was incorporated into the Belgian Congo. A bridge over the Lulua River opened in the town in the late 1950s, shortly before the Democratic Republic of the Congo gained its independence. Transport. The town is on the N20 highway, and is served by Luebo Airport.

Geographic entities mentioned:
surface_form: Lulua River
instance_of: Watercourse
countries: Democratic Republic of the Congo
coordinates: lat: -5.04111111
lon: 21.11194444
Location. Nearby amenities include the BMX bike park, City Centre Aquatic Complex, Coquitlam City Hall, Coquitlam RCMP and Fire Department, Coquitlam Town Centre, Douglas College (David Lam campus), Evergreen Cultural Centre, Lafarge Lake, Percy Perry Stadium, Pinetree Secondary School, Town Centre Park, and Tri-Cities Chamber of Commerce. Entrances.

Geographic entities mentioned:
surface_form: Lafarge Lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.287
lon: -122.789
History. This area was once home to the indigenous Kitanemuk tribe, a branch of the Serranos, who lived as hunter/gathers. They were first encountered by Franciscan friar Francisco Garcés in 1776, residing in communal tule houses. They were not a war-like tribe but often fought with the neighboring tribe, the Allikliks on the Santa Clara River.

Geographic entities mentioned:
surface_form: Kitanemuk
instance_of: Valley
countries: United States
Valles Caldera. The Valles Caldera (or Jemez Caldera) is a volcanic caldera in the Jemez Mountains of northern New Mexico. Hot springs, streams, fumaroles, natural gas seeps, and volcanic domes dot the caldera landscape. The highest point in the caldera is Redondo Peak, an resurgent lava dome located entirely within the caldera and surrounded by moat-like flows of rhyolitic solidified lavas.

Geographic entities mentioned:
surface_form: Redondo Peak
instance_of: Mountain
countries: United States
coordinates: lat: 35.871963888889
lon: -106.56057777778
The obsidian was knapped into tools and weapons while wild game was followed and hunted seasonally. Obsidian from the caldera was traded by tribes across much of the Southwest. Eventually, the Spanish, and later Mexican settlers along with the Navajo and other tribes came to the caldera seasonally for grazing livestock. This often resulted in periodic clashes and raids between tribes and cultures.

Geographic entities mentioned:
surface_form: navajo
instance_of: Mountain
countries: United States
coordinates: lat: 37.034169444444
lon: -110.86888888889
Ross, R.L. Smith, and R.A. Bailey during field work at Valles in the 1960s. This type locality and associated studies have been used to studied other resurgent domes around the world, including Yellowstone Caldera. After the initial caldera-forming eruption at Valles, the Redondo Peak resurgent dome was uplifted beginning around 1.2 million years ago.

Geographic entities mentioned:
surface_form: yellowstone
instance_of: Lake
countries: United States
coordinates: lat: 44.466666666667
lon: -110.36666666667
Ross, R.L. Smith, and R.A. Bailey during field work at Valles in the 1960s. This type locality and associated studies have been used to studied other resurgent domes around the world, including Yellowstone Caldera. After the initial caldera-forming eruption at Valles, the Redondo Peak resurgent dome was uplifted beginning around 1.2 million years ago.

Geographic entities mentioned:
surface_form: redondo peak
instance_of: Mountain
countries: United States
coordinates: lat: 35.871963888889
lon: -106.56057777778
Valles Caldera. The Valles Caldera (or Jemez Caldera) is a volcanic caldera in the Jemez Mountains of northern New Mexico. Hot springs, streams, fumaroles, natural gas seeps, and volcanic domes dot the caldera landscape. The highest point in the caldera is Redondo Peak, an resurgent lava dome located entirely within the caldera and surrounded by moat-like flows of rhyolitic solidified lavas.

Geographic entities mentioned:
surface_form: valles caldera
instance_of: Mountain
countries: United States
coordinates: lat: 35.866666666667
lon: -106.56666666667
Valles Caldera. The Valles Caldera (or Jemez Caldera) is a volcanic caldera in the Jemez Mountains of northern New Mexico. Hot springs, streams, fumaroles, natural gas seeps, and volcanic domes dot the caldera landscape. The highest point in the caldera is Redondo Peak, an resurgent lava dome located entirely within the caldera and surrounded by moat-like flows of rhyolitic solidified lavas.

Geographic entities mentioned:
surface_form: valles caldera
instance_of: Mountain
countries: United States
coordinates: lat: 35.866666666667
lon: -106.56666666667
surface_form: jemez caldera
instance_of: Mountain
countries: United States
coordinates: lat: 35.866666666667
lon: -106.56666666667
Located within the caldera are several grass valleys, or &quot;valles&quot;, the largest of which is Valle Grande (), the only one accessible by a paved road. In 1975, Valles Caldera was designated as a National Natural Landmark by the National Park Service with much of the caldera being within the Valles Caldera National Preserve, a unit of the National Park System.

Geographic entities mentioned:
surface_form: valles caldera
instance_of: Mountain
countries: United States
coordinates: lat: 35.866666666667
lon: -106.56666666667
Dunigan bought out the timber rights in the 1970s and slowed the logging. He negotiated unsuccessfully with the National Park Service and the US Forest Service for possible sale of the property in the 1980s. Valles Caldera National Preserve. The Valles Caldera Preservation Act of 2000 signed by President Clinton on July 25, 2000, created the Valles Caldera National Preserve (VCNP).

Geographic entities mentioned:
surface_form: valles caldera
instance_of: Mountain
countries: United States
coordinates: lat: 35.866666666667
lon: -106.56666666667
The preserve is encircled by federal lands, including the Santa Fe National Forest, the Jemez National Recreation Area, and Bandelier National Monument. The Valles Caldera Preservation Act of 2000 also created the Valles Caldera Trust, an experimental management organization consisting of nine board members, including seven appointed by the President of the United States.

Geographic entities mentioned:
surface_form: valles caldera
instance_of: Mountain
countries: United States
coordinates: lat: 35.866666666667
lon: -106.56666666667
The 2011 bill was supported by the VCNP trustees and a majority of New Mexico's Congressional delegation. On December 19, 2014, President Barack Obama signed the 2015 National Defense Authorization Act, which transferred administrative jurisdiction of the preserve from the Valles Caldera Trust to the National Park Service.

Geographic entities mentioned:
surface_form: valles caldera
instance_of: Mountain
countries: United States
coordinates: lat: 35.866666666667
lon: -106.56666666667
After a brief transition period, the National Park Service assumed day-to-day management on October 1, 2015. On October 10, the preserve held an official dedication with dignitaries including U.S. Secretary of the Interior Sally Jewell, U.S. Senator Tom Udall, U.S. Senator Martin Heinrich, former U.S.

Geographic entities mentioned:
surface_form: valles caldera
instance_of: Mountain
countries: United States
coordinates: lat: 35.866666666667
lon: -106.56666666667
Las Conchas Fire. In July 2011, the Las Conchas Fire, started by a power line on nearby private land, burned of the Valles Caldera National Preserve. The wildfire burned a total of in the Jemez Mountains, including most of neighboring Bandelier National Monument.

Geographic entities mentioned:
surface_form: valles caldera
instance_of: Mountain
countries: United States
coordinates: lat: 35.866666666667
lon: -106.56666666667
The Toledo and Valles Calderas formed during eruptions 1.61 million and 1.25 million years ago, respectively. The caldera-forming Toledo eruption emplaced the Otowi member of the Bandelier Tuff 1.61 million years ago, which can be seen along canyon walls west of Valles Caldera, including San Diego Canyon.

Geographic entities mentioned:
surface_form: valles caldera
instance_of: Mountain
countries: United States
coordinates: lat: 35.866666666667
lon: -106.56666666667
The caldera-forming Toledo eruption emplaced the Otowi member of the Bandelier Tuff 1.61 million years ago, which can be seen along canyon walls west of Valles Caldera, including San Diego Canyon. The younger Tshirege Member of the Bandelier Tuff was formed during the Valles Caldera eruption 1.23 million years ago.

Geographic entities mentioned:
surface_form: valles caldera
instance_of: Mountain
countries: United States
coordinates: lat: 35.866666666667
lon: -106.56666666667
The El Cajete Pumice and Battleship Rock Ignimbrite were emplaced in a single eruptive event 74,200 ± 1,100 years ago, followed by the eruption of the Banco Bonito obsidian flow during the youngest eruption of Valles Caldera, at 68,900 ± 1,000 years ago. The caldera and surrounding area continue to be shaped by ongoing volcanic activity.

Geographic entities mentioned:
surface_form: valles caldera
instance_of: Mountain
countries: United States
coordinates: lat: 35.866666666667
lon: -106.56666666667
Notable geologist instructors included Roy Bailey. Climate. According to the Köppen climate classification, Valles Caldera has a subarctic climate (Dfc), with cold winters and mild summers. The caldera is subject to strong temperature inversions, causing very cold nights year round and high diurnal temperature variation. Geothermal energy exploration.

Geographic entities mentioned:
surface_form: valles caldera
instance_of: Mountain
countries: United States
coordinates: lat: 35.866666666667
lon: -106.56666666667
Valles caldera was home to the first experiments into development of an Enhanced geothermal system (EGS) or Hot-dry-rock (HDR) geothermal system, beginning in 1974 by the Los Alamos National Laboratory at the Fenton Hill reservoir, approximately 3 km west of Valles caldera.

Geographic entities mentioned:
surface_form: valles caldera
instance_of: Mountain
countries: United States
coordinates: lat: 35.866666666667
lon: -106.56666666667
Originally, the Fenton Hill site was chosen as an EGS laboratory in hopes that the proximity to Valles caldera would increase the temperature of the bedrock, thus requiring shallower drill depths. The abundance of hydrothermal fluids discharged from the nearby caldera resulted in hydrothermal alteration of the rocks at depth, weakening the sealed nature of the reservoir.

Geographic entities mentioned:
surface_form: valles caldera
instance_of: Mountain
countries: United States
coordinates: lat: 35.866666666667
lon: -106.56666666667