Sarmila/GeoWiki-Features huggingface dataset:
They are near Echo Ridge. John Muir and Echo Peaks. John Muir passed by Echo Peaks, writing about it in &quot;The Yosemite&quot;, sometime during or before 1912. The area. Echo Peaks are near all of Budd Lake, Cathedral Lakes, Cathedral Peak, Cockscomb, Elizabeth Lake, Matthes Crest, Tresidder Peak and Unicorn Peak. Rock climbing. Echos Peaks have rock climbing.

Geographic entities mentioned:
surface_form: budd lake
instance_of: Lake
countries: United States
coordinates: lat: 44.0228
lon: -84.7967
surface_form: cathedral peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.8689
lon: -113.866
surface_form: elizabeth lake
instance_of: Lake
countries: United States
coordinates: lat: 34.6658
lon: -118.403
surface_form: budd lake
instance_of: Lake
countries: United States
coordinates: lat: 37.8417
lon: -119.396
surface_form: unicorn peak
instance_of: Mountain
countries: United States
coordinates: lat: 46.745
lon: -121.7
surface_form: cathedral peak
instance_of: Mountain
countries: United States
coordinates: lat: 37.8477
lon: -119.405
surface_form: cathedral peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.0344
lon: -106.859
surface_form: tresidder peak
instance_of: Mountain
countries: United States
coordinates: lat: 37.8297
lon: -119.422
surface_form: cathedral peak
instance_of: Mountain
countries: United States
coordinates: lat: 42.8253
lon: -109.179
surface_form: budd lake
instance_of: Lake
countries: United States
coordinates: lat: 43.64
lon: -94.46666667
surface_form: cathedral peak
instance_of: Mountain
countries: United States
coordinates: lat: 58.6125
lon: -134.3664
surface_form: cockscomb
instance_of: Mountain
countries: United States
coordinates: lat: 37.83548
lon: -119.3846
surface_form: cathedral lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 37.844994
lon: -119.423954
surface_form: elizabeth lake
instance_of: Lake
countries: United States
coordinates: lat: 42.630489
lon: -83.380641
surface_form: cathedral peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.98926
lon: -120.188954
surface_form: elizabeth lake
instance_of: Lake
countries: United States
coordinates: lat: 48.886
lon: -113.726
surface_form: elizabeth lake
instance_of: Lake
countries: United States
coordinates: lat: 42.50822
lon: -88.26902
surface_form: budd lake
instance_of: Lake
countries: United States
coordinates: lat: 47.16666667
lon: -95.175
surface_form: elizabeth lake
instance_of: Lake
countries: United States
coordinates: lat: 37.845012
lon: -119.370406
surface_form: unicorn peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.01092
lon: -123.52213
Echo Peaks. Echo Peaks consists of nine peaks, in the Tuolumne Meadows region of Yosemite National Park, California. They are near Echo Ridge. John Muir and Echo Peaks. John Muir passed by Echo Peaks, writing about it in &quot;The Yosemite&quot;, sometime during or before 1912. The area.

Geographic entities mentioned:
surface_form: echo peaks
instance_of: Mountain
countries: United States
coordinates: lat: 37.83243
lon: -119.40294
The area. Echo Peaks are near all of Budd Lake, Cathedral Lakes, Cathedral Peak, Cockscomb, Elizabeth Lake, Matthes Crest, Tresidder Peak and Unicorn Peak. Rock climbing. Echos Peaks have rock climbing. Among rock climbers, Echo Peaks are popular, offering class 2-5 climbs on the nine peaklets.

Geographic entities mentioned:
surface_form: echo peaks
instance_of: Mountain
countries: United States
coordinates: lat: 37.83243
lon: -119.40294
Of the agricultural land, 39.4% is used for growing crops and 9.1% is pastures, while 9.1% is used for orchards or vine crops. All the water in the municipality is flowing water. The municipality is located on the left bank of Lake Geneva. Demographics. Corsier has a population () of., 29.1% of the population are resident foreign nationals.

Geographic entities mentioned:
surface_form: Lake Geneva
instance_of: Lake
countries: Switzerland
France
coordinates: lat: 46.45
lon: 6.55
It is located in the boundary of the regions of Huánuco and Pasco. Its summit reaches about above sea level. A lake named Puyhuancocha lies at the northwestern slope of the mountain at. It is located south of Lake Tinquicocha.

Geographic entities mentioned:
surface_form: Lake Tinquicocha
instance_of: Lake
countries: Peru
coordinates: lat: -10.4256
lon: -76.7353
Puyhuanccocha. Puyhuanccocha (possibly from Quechua &quot;puywan&quot; heart of an animal, &quot;qucha&quot; lake, &quot;heart lake&quot;) is a mountain in the Raura mountain range in the Andes of Peru. It is located in the boundary of the regions of Huánuco and Pasco. Its summit reaches about above sea level. A lake named Puyhuancocha lies at the northwestern slope of the mountain at.

Geographic entities mentioned:
surface_form: puywan
instance_of: Mountain
countries: Peru
coordinates: lat: -11.8558
lon: -75.0444
surface_form: puyhuanccocha
instance_of: Mountain
countries: Peru
coordinates: lat: -10.45611111
lon: -76.73611111
surface_form: puywan
instance_of: Mountain
countries: Peru
coordinates: lat: -9.63306
lon: -77.2458
Puyhuanccocha. Puyhuanccocha (possibly from Quechua &quot;puywan&quot; heart of an animal, &quot;qucha&quot; lake, &quot;heart lake&quot;) is a mountain in the Raura mountain range in the Andes of Peru. It is located in the boundary of the regions of Huánuco and Pasco. Its summit reaches about above sea level. A lake named Puyhuancocha lies at the northwestern slope of the mountain at.

Geographic entities mentioned:
surface_form: puyhuanccocha
instance_of: Mountain
countries: Peru
coordinates: lat: -10.45611111
lon: -76.73611111
Polynucleobacter victoriensis. &quot;Polynucleobacter victoriensis&quot; is an aerobic, chemo-organotrophic, non-motile, free-living bacterium of the genus &quot;Polynucleobacter&quot;. The type strain was isolated from Lake Victoria near Kampala in Uganda, East Africa. This strain was previously included in the description of &quot;P.

Geographic entities mentioned:
surface_form: Lake Victoria
instance_of: Lake
countries: Tanzania
Uganda
Kenya
coordinates: lat: -1
lon: 33
The ménage à trois partners lived together in Tigh-na-Crich, Lochearnhead, until Ker moved out in 1939. They lived in a house they named (Sunny Burn), located on Glen Ogle. Holme was a frequent speaker and lecturer for the Women's Rural Institutes, which she, Greenlees and Ker all supported from its creation around 1923.

Geographic entities mentioned:
surface_form: Glen Ogle
instance_of: Valley
countries: United Kingdom
coordinates: lat: 56.408333333333
lon: -4.3125
Isaev, who claimed that Shevchenko was still writing and drawing. Shevchenko was detained in the guardhouse from 27 April to 12 May 1850. Later that year, he was sent to the Novopetrovskoe fortification on the Caspian Sea. The museum was established by the executive committee of the Orenburg City Council (decision No.

Geographic entities mentioned:
surface_form: Caspian Sea
instance_of: Body of water
Lake
countries: Iran
Russia
Kazakhstan
Azerbaijan
Turkmenistan
Russian Empire
Soviet Union
coordinates: lat: 42
lon: 50.5
Many locations have been proposed. Schmidt and Wasson (1993) suggested there could be a, in diameter source crater beneath the Mekong Valley, Hartung and Koeberl (1994) proposed the elongated Tonlé Sap lake in Cambodia, Glass (1994) estimated the source crater to be between in diameter and located in Cambodia, and Schnetzler (1996) suggested a 35–40 km structure in southern Laos.

Geographic entities mentioned:
surface_form: Tonlé Sap lake
instance_of: Lake
countries: Cambodia
coordinates: lat: 12.883333333333
lon: 104.06666666667
More recently in 2020 and again in 2023 Sieh et al. proposed on the basis of various lines of evidence that the crater lies buried beneath the Bolaven volcanic field in southern Laos, and was around in diameter. Another 2023 study alternatively suggested that the crater was buried under sand dunes in the Badain Jaran Desert in northwest China.

Geographic entities mentioned:
surface_form: Bolaven
instance_of: Mountain
countries: Laos
coordinates: lat: 15.11
lon: 106.44
Mina Clavero. Mina Clavero is a municipality in San Alberto Department in Córdoba Province, Argentina. It forms the municipality of same name and is the tourist center of Traslasierra valley. It is characterized by its natural landscapes, beaches and nightlife.

Geographic entities mentioned:
surface_form: Traslasierra valley
instance_of: Valley
countries: Argentina
It is a social species and fish in larger groups fed better than those in smaller groups
Fisheries. &quot;Pomadasys stridens&quot; is not regarded as a food fish in South Africa where it may be caught as a bait fish but it is regarded as a commercially important food fish in the northern Indian Ocean in areas such as the Gulf of Aqaba, Persian Gulf and the Bitter Lakes in Egypt.

Geographic entities mentioned:
surface_form: Bitter Lakes
instance_of: Group of lakes
countries: Egypt
coordinates: lat: 30.268611111111
lon: 32.447222222222
The specific epithet (&quot;foliosa&quot;) means 'leafy' or 'full of leaves'. Distribution and habitat. This species of &quot;Jacksonia&quot; grows in shrubland in sand over laterite between Mount Adams and Wongan Hills in the Avon Wheatbelt, Geraldton Sandplains, Jarrah Forest and Swan Coastal Plain bioregions of south-west of Western Australia. Conservation status.

Geographic entities mentioned:
surface_form: Wongan Hills
instance_of: Mountain
countries: Australia
coordinates: lat: -30.8
lon: 116.617
Cerro del Bolsón. Cerro del Bolsón is a mountain in the Aconquija Range of Argentina, on the border between Catamarca and Tucumán provinces. It is the highest point of a significant eastern spur of the main range of the Andes, east of the Puna de Atacama region. It lies about 200 kilometres east of Ojos del Salado, the highest point in the Puna de Atacama.

Geographic entities mentioned:
surface_form: Ojos del Salado
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.109444444444
lon: -68.542222222222
Cerro del Bolsón. Cerro del Bolsón is a mountain in the Aconquija Range of Argentina, on the border between Catamarca and Tucumán provinces. It is the highest point of a significant eastern spur of the main range of the Andes, east of the Puna de Atacama region. It lies about 200 kilometres east of Ojos del Salado, the highest point in the Puna de Atacama.

Geographic entities mentioned:
surface_form: cerro del bolsón
instance_of: Mountain
countries: Argentina
coordinates: lat: -27.214166666667
lon: -66.094166666667
Lake Pumacocha (Yauli). Pumacocha (possibly from Quechua &quot;puma&quot; cougar, puma, &quot;qucha&quot; lake,) is a lake in Peru located in the Junín Region, Yauli Province, Yauli District. It is situated at a height of approximately, about 5.144 km long and 0.95 km at its widest point.

Geographic entities mentioned:
surface_form: junín
instance_of: Lake
countries: Peru
coordinates: lat: -11.0201
lon: -76.1075
surface_form: pumacocha
instance_of: Lake
countries: Peru
coordinates: lat: -11.78
lon: -75.246388888889
surface_form: yauli
instance_of: Mountain
countries: Peru
coordinates: lat: -11.4992
lon: -76.1297
surface_form: yauli
instance_of: Mountain
countries: Peru
coordinates: lat: -11.4992
lon: -76.1297
surface_form: pumacocha
instance_of: Lake
countries: Peru
coordinates: lat: -13.59944444
lon: -74.0125
surface_form: pumacocha
instance_of: Lake
countries: Peru
coordinates: lat: -11.735833333333
lon: -76.118611111111
Lake Pumacocha (Yauli). Pumacocha (possibly from Quechua &quot;puma&quot; cougar, puma, &quot;qucha&quot; lake,) is a lake in Peru located in the Junín Region, Yauli Province, Yauli District. It is situated at a height of approximately, about 5.144 km long and 0.95 km at its widest point.

Geographic entities mentioned:
surface_form: pumacocha
instance_of: Lake
countries: Peru
coordinates: lat: -11.78
lon: -75.246388888889
surface_form: yauli
instance_of: Mountain
countries: Peru
coordinates: lat: -11.4992
lon: -76.1297
surface_form: pumacocha
instance_of: Lake
countries: Peru
coordinates: lat: -13.59944444
lon: -74.0125
surface_form: lake pumacocha (yauli)
instance_of: Lake
countries: Peru
coordinates: lat: -11.735833333333
lon: -76.118611111111
surface_form: pumacocha
instance_of: Lake
countries: Peru
coordinates: lat: -11.735833333333
lon: -76.118611111111
It is situated at a height of approximately, about 5.144 km long and 0.95 km at its widest point. Pumacocha lies northwest of a lake named Huallacocha (possibly from in Quechua &quot;Wallaqucha&quot;) and southwest of the town of Yauli. The Pumacocha dam was completed in 1942. It is long and high. It is operated by Centromín Perú. The reservoir has a volume of and a capacity of.

Geographic entities mentioned:
surface_form: pumacocha
instance_of: Lake
countries: Peru
coordinates: lat: -11.78
lon: -75.246388888889
surface_form: yauli
instance_of: Mountain
countries: Peru
coordinates: lat: -11.4992
lon: -76.1297
surface_form: pumacocha
instance_of: Lake
countries: Peru
coordinates: lat: -13.59944444
lon: -74.0125
surface_form: pumacocha
instance_of: Lake
countries: Peru
coordinates: lat: -11.735833333333
lon: -76.118611111111
The harvest season lasts from June through January. Most U.S. production is in California, with a smaller percentage of the crop grown in Skagit Valley, Washington, where cool springs, mild summers, and rich soil abounds, and to a lesser degree on Long Island, New York. Total US production is around 32,000 tons, with a value of $27 million. About 80 to 85% of U.S.

Geographic entities mentioned:
surface_form: Skagit Valley
instance_of: Valley
countries: United States
coordinates: lat: 48.5
lon: -122.033
Afon Rhythallt. The River Rhythallt (Welsh: Afon Rhythallt) is a river in Gwynedd, North Wales whose source is Llyn Padarn. It flows in a northwesterly direction past the village of Brynrefail, Gwynedd and changes its name to Afon Seiont downstream of Pont Rhythallt in Llanrug. The Afon Seiont eventually reaches the sea at Caernarfon.

Geographic entities mentioned:
surface_form: Llyn Padarn
instance_of: Lake
countries: United Kingdom
coordinates: lat: 53.12888889
lon: -4.13305556
of Govan. Between them her twin engines were rated at 166 NHP. &quot;Modjeska&quot;. &quot;Modjeska&quot; was an excursion steamer on Lake Ontario. Her first owner was the Hamilton Steamboat Co Ltd, which registered her in Hamilton, Ontario. Her United Kingdom official number was 96058. Her ownership passed to the Niagara Steam Navigation Co Ltd in 1911 and Canada Steamship Lines Ltd in 1915.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
By order of viceroy Mayorga in 1779, Constansó began work on a new powder factory in the pueblo of Santa Fe near Mexico City — a project that lasted over two years. Drafting plans for roadways, he supervised the paving of streets and leveling of paths in Mexico. He served as a consultant on the draining of Lake Chalco to supply water for Mexico City.

Geographic entities mentioned:
surface_form: Lake Chalco
instance_of: Lake
countries: Mexico
coordinates: lat: 19.267
lon: -98.983
The streets of the old town exude a gentle, relaxed, timeless atmosphere, and the carefully positioned street statues and sculptures add a series of surprises to a visit to the old town. The local plan for 'rural tourism' has led to the development of other small visitor centres on the district, the biggest of which is in the Guayadeque ravine.

Geographic entities mentioned:
surface_form: Guayadeque ravine
instance_of: Watercourse
countries: Spain
coordinates: lat: 27.92544400924798
lon: -15.461987925082123
Gora Nevskaya. Gora Nevskaya (, meaning &quot;Nevsky Mountain&quot;), is a mountain in the Omsukchan Range, Kolyma Mountains. Administratively it is part of the Magadan Oblast, Russian Federation. This high mountain is the highest point of the Kolyma Mountains, part of the East Siberian Mountains. The highest point in Magadan Oblast, however, is the highest peak of the Okhandya Range.

Geographic entities mentioned:
surface_form: gora nevskaya
instance_of: Mountain
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 62.2258
lon: 155.4392
In the eastern theatre of the war, the Indian Eastern Naval Command completely isolated East Pakistan by a naval blockade in the Bay of Bengal, trapping the Eastern Pakistani Navy and eight foreign merchant ships in their ports.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
Belknap is the youngest shield volcano in the Cascade arc by far, with rugged, barren lava fields that contrast with the forested fields of older Cascade shields. It lies within the central Oregon segment of the Cascades near the Three Sisters area, which is marked by closely clustered volcanic centers that include, from south to north, Mount Bachelor, the Three Sisters, and Belknap.

Geographic entities mentioned:
surface_form: Mount Bachelor
instance_of: Mountain
countries: United States
coordinates: lat: 43.979166666667
lon: -121.68833333333
surface_form: bachelor
instance_of: Mountain
countries: United States
coordinates: lat: 43.979166666667
lon: -121.68833333333
surface_form: mount bachelor
instance_of: Mountain
countries: United States
coordinates: lat: 43.979166666667
lon: -121.68833333333
surface_form: three sisters
instance_of: Mountain
countries: United States
coordinates: lat: 34.5968
lon: -83.9444
surface_form: three sisters
instance_of: Mountain
countries: United States
coordinates: lat: 34.5968
lon: -83.9444
surface_form: three sisters
instance_of: Landform
countries: United States
coordinates: lat: 41.7446
lon: -121.473
surface_form: three sisters
instance_of: Landform
countries: United States
coordinates: lat: 41.7446
lon: -121.473
surface_form: three sisters
instance_of: Mountain
countries: United States
coordinates: lat: 33.8697
lon: -117.359
surface_form: three sisters
instance_of: Mountain
countries: United States
coordinates: lat: 33.8697
lon: -117.359
There are at least 466 Quaternary volcanoes in the Sisters Reach, including several aligned segments of volcanic vents and rare eruptive units of rhyolite (uncommon elsewhere in the Cascade arc). Between the North Sister and Three Fingered Jack volcanoes, Holocene volcanism has been intense, with at least 125 volcanic centers becoming active between 4,000 and 1,300 years ago.

Geographic entities mentioned:
surface_form: Three Fingered Jack
instance_of: Mountain
countries: United States
coordinates: lat: 44.478965122
lon: -121.843058797
Deposits from Belknap buried older lava flows from the Sand Mountain Volcanic Field as well as a series of four cinder cones located about to the southwest of Mount Washington. There are also deposits from Belknap in the Lake Valley region between Belknap and both Sims Butte and Mount Mazama. There are hot springs, known as the Belknap Hot Springs, on the northern bank of the McKenzie River.

Geographic entities mentioned:
surface_form: Mount Mazama
instance_of: Mountain
countries: United States
coordinates: lat: 42.9165186
lon: -122.0844711
surface_form: mount mazama
instance_of: Lake
countries: United States
coordinates: lat: 42.943611111111
lon: -122.10666666667
surface_form: mazama
instance_of: Mountain
countries: United States
coordinates: lat: 42.9165186
lon: -122.0844711
surface_form: mount mazama
instance_of: Mountain
countries: United States
coordinates: lat: 42.9165186
lon: -122.0844711
In total, the Belknap shield and its multiple vents were formed in less than 1,500 years, which was a comparable effusion rate to the Nash Crater scoria cone, the Sand Mountain Volcanic Field, and the Mount Bachelor chain. Eruption rates for Belknap were high, at per 1,000 years, similar to the buildup of rhyodacite before the climactic eruption at Mount Mazama.

Geographic entities mentioned:
surface_form: mount mazama
instance_of: Lake
countries: United States
coordinates: lat: 42.943611111111
lon: -122.10666666667
surface_form: mazama
instance_of: Mountain
countries: United States
coordinates: lat: 42.9165186
lon: -122.0844711
surface_form: mount mazama
instance_of: Mountain
countries: United States
coordinates: lat: 42.9165186
lon: -122.0844711
In total, the Belknap shield and its multiple vents were formed in less than 1,500 years, its last eruptive episode finishing about 1,500 years ago. Belknap formed on the lower slopes of Mount Washington, a highly eroded volcano, and is one of the larger mafic (rich in magnesium and iron) volcanoes in the Sisters Reach.

Geographic entities mentioned:
surface_form: the sisters
instance_of: Mountain
countries: United States
coordinates: lat: 36.331111111111
lon: -115.68388888889
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 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 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
There are a number of subfeatures including the Inaccessible Cones, Little Belknap, South Belknap, and Twin Craters, as well as the Belknap hot springs. Postglacial, mafic eruptions are more common in the Sisters Reach — which includes Belknap — than anywhere in the Cascade volcanic arc.

Geographic entities mentioned:
surface_form: the sisters
instance_of: Mountain
countries: United States
coordinates: lat: 36.331111111111
lon: -115.68388888889
Known as the Sisters Reach, the cluster abruptly broadens first to a width of then to as it approaches its southern end, running for about in length. There are at least 466 Quaternary volcanoes in the Sisters Reach, including several aligned segments of volcanic vents and rare eruptive units of rhyolite (uncommon elsewhere in the Cascade arc).

Geographic entities mentioned:
surface_form: the sisters
instance_of: Mountain
countries: United States
coordinates: lat: 36.331111111111
lon: -115.68388888889
Belknap was the last volcano to erupt in the Three Sisters area. Basaltic andesite dominates the eruptive material in the local mafic volcanoes, which range from early Pleistocene to Holocene age. Belknap is one of the larger mafic volcanoes in the Sisters Reach, more than 30 of which run continuously along the segment.

Geographic entities mentioned:
surface_form: the sisters
instance_of: Mountain
countries: United States
coordinates: lat: 36.331111111111
lon: -115.68388888889
In 1862, the Scott brothers and colleagues formed the McKenzie Fork Wagon Road Company to create a better road passing over lava fields in the area, then later the McKenzie River Wagon Road Company, which had as its objective a road that crossed the Cascade Range near the Three Sisters volcano complex at the Deschutes River.

Geographic entities mentioned:
surface_form: three sisters
instance_of: Mountain
countries: United States
coordinates: lat: 34.5968
lon: -83.9444
surface_form: three sisters
instance_of: Landform
countries: United States
coordinates: lat: 41.7446
lon: -121.473
surface_form: three sisters
instance_of: Mountain
countries: United States
coordinates: lat: 33.8697
lon: -117.359
Belknap Crater's lava flows were produced from its northeastern base and extended to the west, reaching the McKenzie River valley. These events represent one of the largest periods of recent volcanism in the Cascade Range, and were comparable in terms of effusion rates to the formation of Mount Bachelor.

Geographic entities mentioned:
surface_form: bachelor
instance_of: Mountain
countries: United States
coordinates: lat: 43.979166666667
lon: -121.68833333333
surface_form: mount bachelor
instance_of: Mountain
countries: United States
coordinates: lat: 43.979166666667
lon: -121.68833333333
Erosion has altered the area downstream from these falls to a lateral terrace on the wall of the McKenzie Canyon, above the river water level. In total, the Belknap shield and its multiple vents were formed in less than 1,500 years, which was a comparable effusion rate to the Nash Crater scoria cone, the Sand Mountain Volcanic Field, and the Mount Bachelor chain.

Geographic entities mentioned:
surface_form: bachelor
instance_of: Mountain
countries: United States
coordinates: lat: 43.979166666667
lon: -121.68833333333
surface_form: mount bachelor
instance_of: Mountain
countries: United States
coordinates: lat: 43.979166666667
lon: -121.68833333333
surface_form: sand mountain
instance_of: Mountain
countries: United States
coordinates: lat: 30.5592
lon: -85.5261
surface_form: sand mountain
instance_of: Mountain
countries: United States
coordinates: lat: 34.45
lon: -86
surface_form: sand mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.3085
lon: -118.397
surface_form: sand mountain
instance_of: Mountain
countries: United States
coordinates: lat: 35.453333333333
lon: -88.463333333333
Within the last 15,000 years, Cascades volcanoes have erupted about of material excluding rear-arc volcanoes. Of this, about (21 percent) came from 63 distributed or peripheral cones, shields, or mafic and intermediate composition chains, with Belknap and Mount Bachelor contributing 71 percent of that material.

Geographic entities mentioned:
surface_form: bachelor
instance_of: Mountain
countries: United States
coordinates: lat: 43.979166666667
lon: -121.68833333333
surface_form: mount bachelor
instance_of: Mountain
countries: United States
coordinates: lat: 43.979166666667
lon: -121.68833333333
Other nearby mafic eruptive units occur at Sims Butte, Cayuse Crater, LeConte Crater, Mount Bachelor, the Egan Cone cluster, and the Katsuk-Talapus chain, which likely were all emplaced between 18,000 and 8,000 years ago. At the south of Sisters Reach, there is a postglacial, basalt lava flow that lies on the eastern flank of Sitkum Butte (a cone that is older than this lava flow).

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Belknap Crater. Belknap Crater is a shield volcano in the Cascade Range in the U.S. state of Oregon. Located in Linn County, it is associated with lava fields and numerous subfeatures including the Little Belknap and South Belknap volcanic cones. It lies north of McKenzie Pass and forms part of the Mount Washington Wilderness.

Geographic entities mentioned:
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countries: United States
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countries: United States
coordinates: lat: 38.9149
lon: -114.309
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coordinates: lat: 40.4271
lon: -80.0112
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lon: -71.303483333333
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countries: United States
coordinates: lat: 47.4259
lon: -121.7
One important distinction is that almost all vent patterns in the area except the supposed Belknap–Blue Lake alignment individually trend north–south, no matter the alignment of the aggregate trend. Belknap formed on the lower slopes of Mount Washington, a highly eroded volcano; Mount Washington's pinnacle lies about from Belknap.

Geographic entities mentioned:
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coordinates: lat: 47.616666666667
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coordinates: lat: 42.1019
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coordinates: lat: 40.4271
lon: -80.0112
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countries: United States
coordinates: lat: 44.270827777778
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countries: United States
coordinates: lat: 44.3321
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coordinates: lat: 47.4259
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Belknap formed on the lower slopes of Mount Washington, a highly eroded volcano; Mount Washington's pinnacle lies about from Belknap. Dissolved magmatic carbon dioxide flux at Mount Washington and Belknap Crater was calculated by James et al. (1999) to be per year. Belknap consists of a shield volcano and pyroclastic cone, which form a late Holocene shield volcano complex.

Geographic entities mentioned:
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lon: -121.839
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Belknap is well-preserved and serves as a good example of Holocene-era activity in the High Cascades. Its core consists of cinder, which is surrounded by a broad shield. It marks an intermediate scale between cinder cones that produced small lava flows such as Twin Craters or Yapoah and larger volcanoes like Mount Washington or Three Fingered Jack.

Geographic entities mentioned:
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coordinates: lat: 44.270827777778
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coordinates: lat: 47.4259
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Belknap's ash deposits are recognizable by their dark color among road cuts and at near the base of lava flow margins. Notable vents and subfeatures. Little Belknap shield, formed about 3,000 years ago, sits to the right of a high scoria cone of the main Belknap Crater vent, with Mount Washington located to the right of both cones. It is about east of Belknap shield's summit craters.

Geographic entities mentioned:
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countries: United States
coordinates: lat: 47.616666666667
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instance_of: Mountain
countries: United States
coordinates: lat: 47.4259
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There is a glaciated steptoe (island) in the western part of the Belknap lava field. Deposits from Belknap buried older lava flows from the Sand Mountain Volcanic Field as well as a series of four cinder cones located about to the southwest of Mount Washington. There are also deposits from Belknap in the Lake Valley region between Belknap and both Sims Butte and Mount Mazama.

Geographic entities mentioned:
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instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
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countries: United States
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coordinates: lat: 38.9149
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One important distinction is that almost all vent patterns in the area except the supposed Belknap–Blue Lake alignment individually trend north–south, no matter the alignment of the aggregate trend. Belknap formed on the lower slopes of Mount Washington, a highly eroded volcano; Mount Washington's pinnacle lies about from Belknap.

Geographic entities mentioned:
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coordinates: lat: 27.4354
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Belknap's summit cone rises about above the base shield volcano, and the volcano itself rises about above its surroundings. Oregon Route 242, which follows the course of the McKenzie River, passes through the lava fields produced by Belknap Crater, the Yapoah cinder cone volcano, and a number of other volcanic vents. These fields consist of black, basaltic lava and encompass an area of. Ecology.

Geographic entities mentioned:
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The Oregon Skyline Trail, which runs to the west of Belknap's lava flows, follows paths used by Native American populations, who harvested huckleberries in the area. Recreation. The Dee Wright Observatory was built with lava blocks from the lava fields produced by Belknap, Yapoah cinder cone, and other volcanoes. It offers views of local volcanoes; Belknap lies to the north.

Geographic entities mentioned:
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There are clear trends among volcanic centers in the area including at Sand Mountain and Inaccessible Cone, suggesting underlying faults; according to Taylor (1965), Belknap's alignment with the Spatter Cone Chain and Blue Lake Crater might similarly indicate underlying faults or fractures connecting the vents at depth, though there are some irregularities.

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Its lava flows encompass about. It has a pyroclastic core. The more southern of the two craters on Belknap's summit cone has a depth of and width of more than at its rim. Belknap is one of three major lava fields in its area with Sand Mountain and Yapoah–Four-in-One–Collier. Of these, Belknap is the largest, encompassing Belknap Crater's shield, Little Belknap, and South Belknap cone.

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Besides the volcanic vents related to Belknap Crater, there are two volcanoes south of Belknap which were also recently active: Four-in-One Cone and Collier Cone. Another, unnamed cone at the northern end of Inaccessible Cone's alignment, which rises to a height of, was breached on its western and southwestern sides by gray basalt lava, which is older than Sand Mountain Volcanic Field and Belknap.

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Eruptions during a subsequent phase about 2,900 years ago built a smaller shield volcano, Little Belknap. According to Sherrod et al. (2004), lava from Little Belknap formed a tree mold in the southern part of the Sand Mountain volcanic field, which was dated to 2,883 ± 175 years Before Present (B.P.) via radiocarbon dating. Sherrod et al.

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The lava that moved south crossed over more ancient lava from Twin Craters, while the lava that ran to the west covered lava and cinder cones within the Inaccessible Cone lineament. The west-moving lavas also moved over Sand Mountain lava flows (erupted from the southern group of vents and the southern vent of Sand Mountain itself), entering the McKenzie Canyon.

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Recent activity and potential hazards. Postglacial, mafic eruptions are more common in the Sisters Reach — which includes Belknap — than anywhere in the Cascade volcanic arc. A lava flow lies next to South Cinder Peak, the Nash Crater–Lost Lake cone cluster, Sand Mountain Volcanic Field, Inaccessible Cone chain, Blue Lake Crater, and a number of monogenetic scoria cones and chains.

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He observed only sparse growth of trees on lava flows from Little Belknap in a report published in the 1980s, noting that soil from Belknap was about thick and made up of lapilli and volcanic ash, which came mostly from Belknap Crater. Along the trail to Little Belknap Crater, there is a tree island with lodgepole pine, mountain hemlock, and true fir.

Geographic entities mentioned:
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Early lava flows near South Belknap were covered by a later lava flow, which was produced by a vent located about northwestward. This lava flow also overlapped with the western part of Belknap Crater's lava, and then it reached Lake Valley, where it formed the northern shore of the local Hand Lake. A deposit of alluvium abuts the margin of South Belknap's lava deposits.

Geographic entities mentioned:
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Belknap Crater. Belknap Crater is a shield volcano in the Cascade Range in the U.S. state of Oregon. Located in Linn County, it is associated with lava fields and numerous subfeatures including the Little Belknap and South Belknap volcanic cones. It lies north of McKenzie Pass and forms part of the Mount Washington Wilderness.

Geographic entities mentioned:
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coordinates: lat: 44.284943458
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The Oregon Skyline Trail, which runs to the west of Belknap's lava flows, follows paths used by Native American populations, who harvested huckleberries in the area. Today, there are a number of trails that run near Belknap, including ones that extend to Little Belknap and Belknap Crater.

Geographic entities mentioned:
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coordinates: lat: 44.284943458
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Today, there are a number of trails that run near Belknap, including ones that extend to Little Belknap and Belknap Crater. Belknap can be seen by tourists at the Dee Wright Observatory, which was built in-part with lava blocks from Belknap Crater. A precise determination for Belknap's age has not been made, as its early history remains obscure.

Geographic entities mentioned:
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coordinates: lat: 44.284943458
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Belknap has likely been built up by eruptive activity over a long period of time. Belknap Crater has had four Holocene eruptive periods confirmed by geological evidence. In total, the Belknap shield and its multiple vents were formed in less than 1,500 years, its last eruptive episode finishing about 1,500 years ago.

Geographic entities mentioned:
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However, the Volcano Hazards Program of the United States Geological Survey considers it unlikely that Belknap will erupt again soon. Geography. Belknap Crater lies to the north of the Three Sisters, in the U.S. state of Oregon. Located within Linn County, it is part of the central Oregon segment of the Cascade Range. L. A. McArthur and L. L.

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