The south pole of
Enceladus is tectonically active today. We can see the tectonic
activity as it
occurs. Four deep, parallel 'tiger paw" groves are active water
volcanoes. The Cassini spacecraft
photographed the plumes from several angles and lighting conditions as
they spew ice mist into
space. Here is a mosaic of the plumes taken with the Sun shining
through the jets. Credit: NASA / JPL / SSI,
mosaic by Emily Lakdawalla
from the
Planetary Society. Click here
to see a larger version of Emily's imagine. http://planetary.org/image/N00146851_55_rotated_mosaic.png
A heat map shows that the four
rift valleys are warmer than the surrounding surface. This suggests
that warm waters are seeping up through cracks
in the ice. Since Enceladus orbits in the densest part of Saturn's F
ring,
evidently the ring was formed
from the moon's tectonic activity. The area between Enceladus' tiger
paws is also covered with
steep canyons. These canyons shows evidence that the tectonic features
were
once much closer
together - that they continually spread apart.