Ruach Planitia
   HOME

TheInfoList



OR:

Ruach Planitia is a roughly circular flat plain and probable cryolava lake on
Neptune Neptune is the eighth and farthest known planet from the Sun. It is the List of Solar System objects by size, fourth-largest planet in the Solar System by diameter, the third-most-massive planet, and the densest giant planet. It is 17 t ...
's moon
Triton Triton commonly refers to: * Triton (mythology), a Greek god * Triton (moon), a satellite of Neptune Triton may also refer to: Biology * Triton cockatoo, a parrot * Triton (gastropod), a group of sea snails * ''Triton'', a synonym of ''Triturus' ...
. It is located in Triton's northern hemisphere within Monad Regio and directly borders the cryovolcanic plains of Cipango Planum to the east and Tuonela Planitia to the west. Ruach Planitia, along with the other three walled plains of Triton, is one of the youngest and flattest features observed on the moon.


Discovery and naming

Ruach Planitia was discovered alongside Triton's other surface features by the ''
Voyager 2 ''Voyager 2'' is a space probe launched by NASA on August 20, 1977, as a part of the Voyager program. It was launched on a trajectory towards the gas giants (Jupiter and Saturn) and enabled further encounters with the ice giants (Uranus and ...
'' spacecraft during its flyby of the
Neptune Neptune is the eighth and farthest known planet from the Sun. It is the List of Solar System objects by size, fourth-largest planet in the Solar System by diameter, the third-most-massive planet, and the densest giant planet. It is 17 t ...
system on 25 August 1989. The name Ruach Planitia was approved by the
International Astronomical Union The International Astronomical Union (IAU; , UAI) is an international non-governmental organization (INGO) with the objective of advancing astronomy in all aspects, including promoting astronomical research, outreach, education, and developmen ...
(IAU) in 1991; it is named after the legendary French isle of
Ruach In Judaism, the Holy Spirit (, ''ruach ha-kodesh'') is conceived of as the divine force, quality, and influence of God in Judaism, God over the universe or over God's creatures, in given contexts.Maimonides, Moses. Part II, Ch. 45: "The various ...
.


Geology

Ruach Planitia is quasi-circular in shape and some 175–180 km in diameter. The floor of Ruach Planitia is depressed by about 200 meters relative to the surrounding plains, with the floor surrounded by bounding scarp that ranges in height between 40 and 250 meters. Most of Ruach Planitia is surrounded by a single bounding scarp, but on its east side the scarp appears to separate into two, giving a terraced profile. The floor of Ruach Planitia is generally flat, but may be subtly warped; given the limitations of ''Voyager 2'' elevation data in the region, whether or not these are artifacts or true elevation features is uncertain. The central region of Ruach Planitia is significantly more varied in topography compared to much of Ruach Planitia's floor, with a large central pit—Dilolo Patera— (Center Latitude: 26.00°, Center Longitude: 24.50°) nearly 10 km wide and roughly 350 m deep. Dilolo Patera is surrounded by a network of smaller pits, linear troughs, and scarps. The pit cluster at Ruach Planitia is similar to the pit clusters found within the other three walled plains of Triton, with only a single pit cluster with the largest pit at the center of the plains. Both Ruach Planitia and nearby Tuonela Planitia cut into the surrounding cantaloupe terrain, and Ruach Planitia cuts into the western regions of Cipango Planum. Ruach Planitia's terraced appearance resembles that of terrestrial volcanic
caldera A caldera ( ) is a large cauldron-like hollow that forms shortly after the emptying of a magma chamber in a volcanic eruption. An eruption that ejects large volumes of magma over a short period of time can cause significant detriment to the str ...
s, albeit at a very large scale. As with terrestrial calderas, eruptions from Ruach Planitia may have involved several distinct stages, with an early explosive stage of high-viscosity or high-volatility
cryolava A cryovolcano (sometimes informally referred to as an ice volcano) is a type of volcano that erupts gases and volatile material such as liquid water, ammonia, and hydrocarbons. The erupted material is collectively referred to as ''cryolava''; ...
, a term for erupted water-dominated material analogous to silicate
lava Lava is molten or partially molten rock (magma) that has been expelled from the interior of a terrestrial planet (such as Earth) or a Natural satellite, moon onto its surface. Lava may be erupted at a volcano or through a Fissure vent, fractu ...
. These early eruptions form the terraced walls, with a later effusive stage that forms the flat floor. However, the crenulated appearance of the walls of Ruach Planitia do not appear to indicate collapse, and instead resemble eroded shorelines found on
Earth Earth is the third planet from the Sun and the only astronomical object known to Planetary habitability, harbor life. This is enabled by Earth being an ocean world, the only one in the Solar System sustaining liquid surface water. Almost all ...
. The multiple terraces on Ruach Planitia's eastern side may have arisen from compositional differences in different layers of Triton's crust, with some layers being more volatile than others. The flat floor of Ruach Planitia suggests that fluid cryolava infilled the depression, with the pits around Dilolo Patera acting as central vents whence material erupted from. The terrain surrounding Ruach Planitia appears to be significantly modified, with apparent glaciation. The cliffs of both Ruach Planitia and Tuonela Planitia appear to have been significantly eroded, with the north wall of Ruach Planitia apparently having been breached in at least three sites. The breach connects to an apparent channel system that stretches for at least ~230 km, though it extended beyond Triton's terminator and into the unimaged regions of Triton's night side at the time of ''Voyager 2''s visit. It remains uncertain on which direction fluids may have flown within the channel, though tentative deposit features on the north floor of Ruach Planitia may indicate that material flowed into the plains, depositing eroded material onto the floor. Several smaller subcircular depressions are located nearby Ruach Planitia to the south and southwest; these subcircular depressions may be of cryovolcanic origin or from
diapir A diapir (; , ) is a type of intrusion in which a more mobile and ductilely deformable material is forced into brittle overlying rocks. Depending on the tectonic environment, diapirs can range from idealized mushroom-shaped Rayleigh–Taylor ...
ism.


References

{{Triton Surface features of Neptune's moons Extraterrestrial plains Triton (moon)