Dawn's main objective is to characterize
two of the largest bodies in the main asteroid
belt: asteroid Vesta and dwarf planet Ceres. This will
provide important information about the conditions
and processes of the solar system's earliest epoch, as
these protoplanets remaining practically intact since
they were formed.
Despite Ceres is only slightly farther from the Sun
than Vesta, these objects have followed a very different
evolutionary path as a consequence of the diversity
of processes that operated during the first stages of
solar system evolution. Thus, although no meteorites
have been linked to this dwarf planet, the detection of
a possible signature of hydrated minerals reveals that
water seems to have played an important role in the
evolution of Ceres. However, Vesta appears to be a
dry, differentiated body, with evidence of lava flows.
Telescopic observations reveal also the existence of an
impact crater with a diameter of about 460 km near its
south pole. The event that generated this crater may
have excavated about 1% of Vesta. In fact, this catastrophic
event is believed to be responsible for the existence
on Earth of fragments of Vesta. Thus, although
no samples of Ceres are currently available, meteorites
coming from Vesta are known to exist. These achondrites
are magmatic rocks known as HEDs for their
principal constituents: howardites, eucrites and diogenites.
The arrival of Dawn to Vesta on July 2011 offers
an excellent opportunity for education and outreach.
Thus, an exhibition was organized with the aim to
promote the public's interest for the Dawn mission and
the role that meteorites play for our knowledge of
Vesta and other bodies of the Solar System. This outreach
activity was entitled "Vesta and Ceres: the Origins
of the Solar System" (Fig. 1). It took place between
October 2011 and January 2012.