Chimborazo (volcano) in the context of "Elevation"

⭐ In the context of Elevation, Chimborazo is considered notable because…

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⭐ Core Definition: Chimborazo (volcano)

Chimborazo (Spanish: [tʃimboˈɾaso] ) is a stratovolcano in Ecuador and the Cordillera Occidental range of the Andes. Its last known eruption is believed to have occurred around AD 550. Although not the tallest mountain in the Andes or on Earth relative to sea level, its summit is the farthest point on Earth's surface from the Earth's center due to its location along the planet's equatorial bulge. Chimborazo's height from sea level is 6,263 m (20,548 ft), well below that of Mount Everest at 8,849 m (29,031 ft).

Chimborazo is the highest mountain in Ecuador and the 39th-highest peak in the entire Andes. It is a popular destination for mountaineering due to its challenging climbing routes, which involve traversing snow, ice, and rocky terrain.

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👉 Chimborazo (volcano) in the context of Elevation

The elevation of a geographic location is its height above or below a fixed reference point, most commonly a reference geoid, a mathematical model of the Earth's sea level as an equipotential gravitational surface (see Geodetic datum § Vertical datum).The term elevation is mainly used when referring to points on the Earth's surface, while altitude or geopotential height is used for points above the surface, such as an aircraft in flight or a spacecraft in orbit, and depth is used for points below the surface.

Elevation is not to be confused with the distance from the center of the Earth. Due to the equatorial bulge, the summits of Mount Everest and Chimborazo have, respectively, the largest elevation and the largest geocentric distance.

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Chimborazo (volcano) in the context of Aeolian processes

Aeolian processes, also spelled eolian, pertain to wind activity in the study of geology and weather and specifically to the wind's ability to shape the surface of the Earth (or other planets). Winds may erode, transport, and deposit materials. They are effective agents in regions with sparse vegetation, a lack of soil moisture and a large supply of unconsolidated sediments. Although water is a much more powerful eroding force than wind, aeolian processes are important in arid environments such as deserts.

The term is derived from the name of the Greek god Aeolus, the keeper of the winds.

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Chimborazo (volcano) in the context of Cordillera Occidental (Ecuador)

The Cordillera Occidental range is one of two main mountain ranges in the Andes in Ecuador, the other being the Cordillera Central. It spans the whole country from north to south. The highest peak of the Cordillera Occidental is Chimborazo (6,267 metres (20,561 ft)). The range extends from south to north dividing from the Colombian Massif in Nariño Department, passes north through Cauca, Valle del Cauca, Risaralda, Chocó, and Caldas Departments to the Paramillo Massif in Antioquia and Córdoba Departments.

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LINKED FROM (PARENTS)
← Elevation ← Aeolian processes ← Aeolian erosion ← Cordillera Occidental (Ecuador)
LINKS TO (CHILDREN)
Stratovolcano → Ecuador → Cordillera Occidental (Ecuador) → Andes → Types of volcanic eruptions → Sea level → Equatorial bulge → Mount Everest → Mountaineering →