Isluga
Isluga is a stratovolcano located in Colchane, west of the Chile- Bolivia border and at the west end of a group of volcanoes lined up in an east- west direction, which also includes the volcanoes Cabaray and Tata Sabaya.
Isluga has an elongated summit area and lies within the borders of Volcán Isluga National Park in Chile's Tarapacá Region.
Haynes Mountain
Haynes Mountain is a mountain located in the Catskill Mountains of New York south- southwest of Pine Hill.
Haynes Mountain is located south of Belle Ayr Mountain, south- southeast of Hirams Knob, and north of Eagle Mountain.
Cabaray
Cabaraya is a stratovolcano in Bolivia.
It lies between the volcanoes Isluga and Tata Sabaya, immediately east of the border with Chile.
North Fork Mountain
North Fork Mountain is a quartzite- capped mountain ridge in the Ridge and Valley physiographic province of the Allegheny Mountains( or" High Alleghenies" or" Potomac Highlands") of eastern West Virginia, USA.
Kile Knob, at 4,588 feet( 1,398 m), is the mountain's highest point, and Panther Knob and Pike Knob are nearly as high.
North Fork Mountain is the driest high mountain in the Appalachians, and has vegetation and flora different from nearby, wetter high mountain areas immediately to the west such as Spruce Knob and Dolly Sods, with pines(" Pinus") abundant on the mountain's ridgecrest, in contrast with the spruces(" Picea") so characteristic of these comparably high summits across the North Fork Valley.
Structurally, North Fork Mountain is an anticline mountain, a major part of the Wills Mountain Anticline system.
The mountain's strata( rock layers) are nearly flat, but the Tuscarora quartzite that forms the mountain's caprock is bent downwards( and now mostly eroded away) east and west of the ridge, becoming nearly vertical along the mountain's slopes, where the same quartzite stratum forms such dramatic outcrops as Seneca Rocks.
Much of the mountain is within the Monongahela National Forest, and a large portion of the mountain has been proposed for federal wilderness designation or inclusion within a new unit of U.S. National Park System.
The Nature Conservancy's Panther Knob and Pike Knob preserves are also located on North Fork Mountain.
The scenic North Fork Mountain Trail follows much of the ridge crest, and only one road( U.S. Route 33) crosses the steep, rugged ridge.
Pine Knob (disambiguation)
Pine Knob and Pineknob may refer to:
Cabaray
Cabaraya is a stratovolcano in Bolivia.
It lies between the volcanoes Isluga and Tata Sabaya, immediately east of the border with Chile.
Inka Qhamachu
Inka Qhamachu( Quechua" Inka" Inca," qhamachu" a species of wild tobacco"( Nicotiana glauca)", Hispanicized names" Inca Camacho, Incacamachi") is a mountain in the Andes of Bolivia.
It is located in the Oruro Department, Litoral Province, Huachacalla Municipality.
Inka Qhamachu lies southeast of Pacha Qullu, southeast of the village of Huachacalla( Wachaqalla).
Inka Qhamachu is part of the Altiplano, an area of the Andes lying at altitudes of.
The Altiplano has been affected by volcanic activity.
Most of it including Inka Qhamachu is extinct, but in the Western Cordillera volcanic activity persists at Cerro Quemado, Guallatiri, Parinacota, Sajama and Tata Sabaya.
Inka Qhamachu is a Pliocene age volcano, which rises from an altitude of.
Its slopes range 11 – 16 °, formed by lava flows and pyroclastic material.
Erosion has carved radial gullies into its flanks, at whose ends alluvial fans have formed.
Based on the degree of erosion, an age of 7.5 million years has been estimated.
The volume of the edifice once was about.
Temperatures in the closely located city of Oruro range, and precipitation is.
The area is very windy.
This climate has led to a xerophytic vegetation, including shrubs and tussock grass.
Cottle Knob
Cottle Knob is a summit in West Virginia, in the United States.
With an elevation of, Cottle Knob is the 348th highest summit in the state of West Virginia.
Cottle Knob was named after C. W. Cottle, a pioneer hunter.
Tata Sabaya
Tata Sabaya is a high volcano in Bolivia.
It is part of the Central Volcanic Zone, one of several volcanic belts in the Andes which are separated by gaps without volcanic activity.
This section of the Andes was volcanically active since the Jurassic, with an episode of strong ignimbritic volcanism occurring during the Miocene.
Tata Sabaya lies in a thinly populated region north of the Salar de Coipasa salt pan.
Volcanic activity at Tata Sabaya and elsewhere in the Central Volcanic Zone is the consequence of the subduction of the Nazca Plate beneath the South America Plate.
The volcano has developed along a lineament that separates older crust north of the lineament from younger crust in the south, and the edifice has been formed by andesitic rocks.
The southern flank of Tata Sabaya failed during the latest Pleistocene about 12,000- 12,360 years before present.
Debris from the collapse entered a lake that covered the Salar de Coipasa at that time and formed a deposit with a volume of.
Subsequently, the collapse scar was partly filled in with more recent lava flows and lava domes; one eruption occurred about 6,000 years before present.
Paryani
Paryani( Quechua" parya" reddish; copper; sparrow, Aymara"- ni" a suffix, hispanicized spelling" Pariani") is a volcano in the Andes of Bolivia.
It is located in the Oruro Department, Sabaya Province, Sabaya Municipality.
The cone of Paryani lies at the Salar de Coipasa, south of Pumiri and east of Tata Sabaya.

Question: Are Tata Sabaya and Cottle Knob both located in the same country?
Answer: no