|
|
Snow
from a late return of winter lies in patches on and around the
cone of Monte Timparossa in early May 2000. The densely forested
cone is seen here from near the mountain hut of the same name,
about 1 km to the NNE and nearly 300 m lower |
Mamma
Etna's countless children
Monte Timparossa
NE flank, 15.020907° E, 37.805409° N (S rim of crater)
Summit elevation: 2122 m
|
|
Monte
Timparossa is one of the oldest flank cones of Etna that are still visible
among the products of much more recent eruptions. The shape of the cone
and its summit crater have been degraded by erosion in many thousands
of years. Yet it is a fairly large cone, also because it sits on the upper
crest of a steep slope. It is covered with dense forest on its northern
slopes while there is relatively little vegetation at its summit, which
lies approximately at the tree line. The poorly defined summit crater
is open to the north and probably a lava flow was released through this
breach.
Approximately 1 km NNE of the summit of Monte Timparossa stands one of
the most beautiful mountain huts that hikers can find on Etna's slopes.
This has a kitchen with a gas stove and even a toilet (without flowing
water for flushing, however), which cannot be found in any of the other
mountain huts on Etna. It lies within a beautiful forest but from an old
lava tumulus immediately behind the building one can enjoy a spectacular
panoramic view of the lower portion of the Northeast Rift including the
large cones of Monte Timparossa and the much more recent Monte Nero, formed
in 1646-1647.
I first climbed Monte Timparossa to its summit in mid-August 2002 but
passed nearby on other occasions. The photographs on this page were taken
during the August 2002 visit and during numerous other excursions to the
Monte Nero area between 2000 and 2003.
Continue
to Monte Nero
Return
to the Etna flank cone index |