Europa 441
FIGURE 13 Examples of chaos on Europa. (a) Conamara Chaos exhibits distinct plates of preexisting terrain (see also Fig. 14). (b)
Murias Chaos, a region of fine-textured chaos that has apparently overflowed its margins on one side, depressing the surrounding plains.
(c) The edge of Thrace Macula, showing fine-textured material and a hint of preexisting terrain within, suggesting that the preexisting
plains material has disaggregated in place. Dark plains material from Thrace has embayed the surrounding ridged plains, suggesting
that it was relatively fluid when it was emplaced. (After Prockter et al., 2004.)
as they rise to the surface, causing disaggregation into matrix
material and local flooding by dark, low-viscosity melt.
4.2.2 CHAOS
Chaos regions are areas in which kilometer-scale blocks of
existing ridged plains material have translated and rotated
with respect to one another within a mixed-albedo matrix
of hummocky material (Fig. 13). The matrix material can
be low-lying or high-standing relative to the surrounding
plains. In one area, Conamara Chaos, at least 60% of the
preexisting terrain has been replaced with or converted into
matrix material, and the matrix in part stands above the sur-
roundings. Some of the broken plates have been rotated
and/or moved by as much as several kilometers. These plates
can be reassembled like a jigsaw puzzle, reconstructing por-
tions of preexisting ridges and troughs (Fig. 14), although
much of the original surface has been destroyed.
Chaos regions have been interpreted as places where
Europa’s heat flow has been enhanced, and where local
melt-through of ocean water to the surface may have oc-
curred. In such a model, the blocks are analogous to
FIGURE 14 Broken plates of
material within the hummocky
matrix of Conamara Chaos (left) can
be reconstructed into their original
positions like a jigsaw puzzle, by
matching up older lineaments. This
exercise shows that the plates may
have moved by several kilometers
(arrows show approximate amount
of displacement), indicating that the
matrix material was originally
mobile. Most of the original terrain
is missing, however, and may have
been subsumed or disaggregated
during formation of the chaos.
(After Spaun et al., 1998.)