Different regions on Mars appear to have low-albedo intracrater deposi
ts that have distinct regional thermophysical and/or aeolian dune char
acteristics. Thermal inertia derived from a carefully selected set of
Viking infrared thermal mapper observations of the dark features obtai
ned in 1977-1978 supports this conclusion. The observed similarities a
nd differences among dark intracrater features on Mars is probably a f
unction of the combined influences of sand availability and regional w
ind conditions.