The discovery team followed up their initial identification of Eris with
spectroscopic observations made at the 8 m
Gemini North Telescope in Hawaii on January 25, 2005. Infrared light from the object revealed the presence of
methane ice, indicating that the surface may be similar to that of Pluto, which at the time was the only
TNO known to have surface methane, and of Neptune's moon
Triton, which also has methane on its surface. In 2022, near-infrared spectroscopy of Eris by the
James Webb Space Telescope (JWST) revealed the presence of
deuterated methane ice on its surface, at abundances lower than those in
Jupiter-family comets like
67P/Churyumov–Gerasimenko. Eris's comparatively low deuterium abundance suggests that its methane is not primordial and instead may have been produced from subsurface geochemical processes. Substantial quantities of
nitrogen ice on Eris was also detected by the JWST, and it is presumed to have originated from subsurface processes similar to Eris's likely non-primordial methane. The abundance of nitrogen ice on Eris is estimated to be one-third of that of methane by volume. Unlike the somewhat reddish and variegated surfaces of Pluto and Triton, the surface of Eris appears almost white and uniform. Pluto's reddish color is thought to be due to deposits of
tholins on its surface, and where these deposits darken the surface, the lower albedo leads to higher temperatures and the evaporation of methane deposits. In contrast, Eris is far enough from the Sun that methane can
condense onto its surface even where the albedo is low. The condensation of methane uniformly over the surface reduces any albedo contrasts and would cover up any deposits of red tholins. This methane sublimation and condensation cycle could produce
bladed terrain on Eris, similar to those on Pluto. Alternatively, Eris's surface could be refreshed through
radiogenic convection of a global methane and nitrogen ice glacier, similar to Pluto's
Sputnik Planitia. Spectroscopic observations by the JWST support the idea that Eris's surface is continually refreshing, as no signs of
ethane, a byproduct of
radiolyzed methane, were detected on Eris's surface. Due to the distant and eccentric orbit of Eris, its surface temperature is estimated to vary from about . Even though Eris can be up to three times farther from the Sun than Pluto, it approaches close enough that some of the ices on the surface might warm enough to
sublime to form an
atmosphere. Because methane and nitrogen are both highly
volatile, their presence shows either that Eris has always resided in the distant reaches of the Solar System, where it is cold enough for methane and nitrogen ice to persist, or that the celestial body has an internal source to replenish gas that escapes from its atmosphere. This contrasts with observations of another discovered TNO, , which reveal the presence of
water ice but not methane. == Rotation ==