pluto
atmosphere
- this atmosphere of nitrogen - plutonian summer some N2 sublimates from ice to air, increasing atmospheric pressure. - plutos atmosphere contains N2, Co, methan and hydrogen. - pluto has weather
cthulhu regio
- very old region, many craters and tectonic fractures - bright icy material appears to overlay darker tholin-rich surface material, suggesting glacial flow of young material over the older surface
moons of pluto
5 known moons. the largest is Charon, roughly half the diameter of pluto. - they are not tidally locked - they are spinning a lot
tombaugh rego
bright, crater free region
discovery of pluto
clyde tombaugh discovered pluto
pluto surface (2)
complex surface, with high albedo. surface features show evidence of glaciological, erosional, tectonic, sediment transport,
pluto surface
composed largely of water ice. water is a tough mineral and behaves like rock, forming landscape and eroding into sediment sand / dust
interior of pluto
compromised of water ice covered partially by nitrogen ice, but the internal organization of the world is yet unclear - pluto has a density of 1.9, indicating its made up of about two/thirds rock and one third ice. it is probably differentiated into an ice mantle and rocky core. it is possible pluto has an interior ocean of liquid water.
Cthulul regio
covered in dark material, likely tholin far mixed with ices
bedrock surface
covered with soft nitrogen ice, mixed in places with carbon monoxide and methane ice. darker surface materials are probably ice mixed with frozen tholin material
contact binaries
made up of at least two large masses of ice/rock that have merged gravitationally.
hillary montes and norgay montes
mountains of bright water ice. these mountains show evidence of glacial flow and jumbled terrain suggesting some mountains are actually icebergs
mountains and glaciers
nearby polygon features imply glacial flow of nitrogen ice rafts. nitrogen ice fills craters, demonstrating mass movement or precipitation of snow
pluto the planet
orbits the sun every 248 earth years, highly eccentric orbit that inclines out of the ecliptic plane. has a high albedo, indicating a young, icy surface. rotation is titled 112 degrees, so it rotates in a retrograde direction.
new horizons
performed a successful flyby of the pluto charon system. it took over a year for the probe to send all its recorded mission data to earth.
pluto and charon
pluto is orbited by one large moon, Charon, and at least four much smaller moons. Charon is about half the diameter of pluto, making their mutual orbit more like a double planet system than a planet-moon system. Charon is tidally locked to pluto, so that one side faces pluto all the time.
pluto and neptune
pluto occupies a 2:3 orbital resonance with neptune, meaning that for every 2 pluto orbits, neptune completes 3 orbits.
pluto the kulper belt object
small icy bodies formed during accretion of the solar system, and comprised mostly of ice and rock.
nitrogen slush ocean
sputnik planum might be a vast "ocean" of soft nitrogen ice, crusted with nitrogen ice fields in which float slowly tumbling mountains of water ice.
formation of pluto - charon
they were probably formed by a large impact on pluto, splitting it into two objects
cryovolcanoes
volcanoes that erupt molten ice (liquid water slush). if true, plutos interior is warm enough to create a partial melt of water ammonia ice.
snakeskin terrain
wide regions of pluto are covered in "snakeskin" terrain of fluted knife-sharp ridges, probably formed by wind erosion of water-ice hills over billions of years
sputnik planium
wide, flat region, covered in soft nitrogren ice that can flow glacially