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{{MarsGeo-Mount
{| border="1" cellspacing="0" cellpadding="2" align="right"
! bgcolor="#ffffc0" colspan="2" | '''Pavonis Mons'''
| name = Pavonis Mons
| location = {{coor d|0.8|N|113.4|W|globe:Mars}}
|-
| peak = 8.7 [[miles|mi]]
| align="center" colspan=2 |
| discoverer = [[Mariner 9]] (1971)
|-
| naming = Latin - ''Mount Peacock''
! align="left" | [[Topographical summit|Elevation]]
}}
| 8.7 mi
|-
! align="left" | Location
| [[Tharsis]], [[Mars]]
|-
! align="left" | [[Mountain range|Range]]
| [[Tharsis Montes]]
|-
! align="left" | [[Geographic coordinate system|Coordinates]]
| Equator, 113°W
|-
! align="left" | [[Topographic map|Topo map]]
| [[NASA]]
|-
! align="left" | [[List of mountain types|Type]]
| [[Caldera|Caldera volcano]]
|-
! align="left" | [[Geologic time scale|Age of rock]]
| 40-100 million years
|-
! align="left" | [[Volcano|Last eruption]]
| 25 million years ago?
|-
! align="left" | [[First ascent]]
| n/a
|-
! align="left" | Easiest [[Climbing route|route]]
| n/a
|}


'''Pavonis Mons''' is the middle of three [[volcano]]s (collectively known as [[Tharsis Montes]]) on the [[Tharsis]] bulge near the [[equator]] of the [[planet]] [[Mars (planet)|Mars]]. To its north is [[Ascraeus Mons]], and to its south is [[Arsia Mons]]. The largest volcano in the [[solar system]], [[Olympus Mons]], is to its northwest.
'''Pavonis Mons''' is the middle of three [[volcano]]s (collectively known as [[Tharsis Montes]]) on the [[Tharsis]] bulge near the [[equator]] of the [[planet]] [[Mars (planet)|Mars]]. To its north is [[Ascraeus Mons]], and to its south is [[Arsia Mons]]. The largest volcano in the [[solar system]], [[Olympus Mons]], is to its northwest.

Revision as of 13:35, 22 June 2006

Template:MarsGeo-Mount

Pavonis Mons is the middle of three volcanos (collectively known as Tharsis Montes) on the Tharsis bulge near the equator of the planet Mars. To its north is Ascraeus Mons, and to its south is Arsia Mons. The largest volcano in the solar system, Olympus Mons, is to its northwest.

Pavonis Mons stands at about seven km above the surrounding plain. By comparison, the highest mountain on Earth, Mount Everest, stands about 8.85 km above sea level. To its lower east flank, there is a chain of elliptical, or oval-shaped, pits, lined up down the center of a shallow trough. They were both formed by collapse associated by faulting – the scarp on each side of the trough is a fault line. (Such features are normally found when the ground is moved by molten rock or tectonic forces.)

In fiction

Because of its position on the Martian equator, Pavonis Mons has been used by fiction authors as a likely site for a future space elevator on the planet. This appears in Kim Stanley Robinson's Mars Trilogy (in which Pavonis is also the site of the Martian capital city, Sheffield), and in the GURPS Transhuman Space roleplaying game source book about Mars, In the Well (in which the elevator is called 'Beanstalk', and is linked to the moon Deimos).[1]

In music

See also