|
|
File name |
Description |
 |
The Iceman Crew departs |
First item
of the new day was to say farewell to the intrepid Iceman crew as
they journeyed forth onto the Italian public transportation system
for their five-hour train-ride to Bolzano. I joked at the time that
the picture was for posterity, should they not return. If I only
knew what I was saying... |
 |
The
journey north |
We followed the
autostrada north through the northernmost part of the Apennine
Mountains. The Apennines are a very youthful mountain range that
originated with the subduction of the Adriatic plate beneath the
Italian mainland. The mountains are a sequence of thrust plates that
have been forced over one another as the compressive forces continue
to push the crustal plates together. The rugged mountains, though
not overly high, have long been a barrier to travel, and the
northern and southern parts have long been separate politically and
culturally.
|
 |
Bridge in the Apennines |
The engineers who
designed the highway were forced to build at least 17 tunnels and
countless bridges. |
 |
Outcrop of limestone |
Every so often,
some of the limestone bedrock would peek out...these layers formed
the bottom of a shallow sea just a few million years ago in Miocene
time. They have become the top of a mountain range in a blink of
geologic time. |
 |
Apennine Scene |
The mountains are
quite beautiful, and contain several national parks. The mountains
are still being pushed to the north by tectonic forces. |
 |
Po
River Plain |
We descended onto
the Po River Plain, the largest agricultural region in Italy, and
exceedingly flat...it was very reminiscent of living in California's
Central Valley. The valley has a similar climate, the same problems
with conflicts over river water, groundwater, and
domestic/agricultural competition for scarce resources. The big
difference is geological... |
 |
The
Po River |
The valley is
caught between two major compressional mountain belts, the
Apennines, and the Alps. The two ranges are being pushed towards
each other, and in the fullness of geological time, the valley will
disappear as the mountains collide, forming an even greater mountain
range. We only had
the briefest view of the Po River. Draining both the Alps and the
northernmost Apennines, it is both the largest and most over-used
river in Italy.
|
 |
Entering Verona |
Our next stop was
Verona, the beautiful medieval city nestled against the foothills of
the Alps. Our visit emphasized the historical aspects of the city,
but there were a few noticeable geological aspects to point out... |
 |
The
Adige River |
The Adige River,
for instance, flows out of the Alps, and the cloudy water is not
pollution, but is instead the very fine suspended silt and clay of
glaciers, which are present many miles up the valley. Other rivers
in the southern Alps are impeded by lakes, which work as settling
ponds, so that the water runs clearer downstream. |
 |
Ammonite in Sidewalk |
The local geology
determines the most economical building materials in Verona (and
Venice and other northern Italian cities). The tufa and the volcanic
tuffs are hundreds of miles away, and the most easily utilizable
stone is a unique pinkish marble (stained by iron oxides) that often
reveals fossils. Here, in a sidewalk, is a coiled ammonite fossil.
It is an extinct tentacled creature that can be likened to an
octopus with a coiled shell. |
 |
Approaching the Piazza
dei Signori and Torre Lamberti |
The presence of
clay deposits on the Po Valley Plain provides for the other building
material used extensively in Verona: bricks! As we walked through
the Piazza dei Signori, the Torre Lamberti (tower) came into view. I
found the fact that tower is open to visits irresistible,
and I headed to the entrance, except....that...there was food
in the Piazza! |
 |
Food! |
O.K., nothing
geological here; other than the fact that this is what gave me the
energy to climb the numerous stairs of the Torre Lamberti...and the
Caprese was delicious! |
 |
Climbing the Torre Lamberti |
There was an elevator to the top of the tower, but I
got all self-righteous, and decided to climb the hundreds of stairs.
The Torre
Lamberti was begun in 1172, but
in May 1403, a thunderstorm destroyed the
upper part. An octagonal belfry was added in 1464. The clock was
added only in 1779. At 276 feet (84 meters),
it is the tallest building in
Verona. The view was marvelous! |
 |
View from the Torre Lamberti |
Looking over the
south end of the Piazza della Erbe and towards the Po River plains. |
 |
View east from the Torre Lamberti |
Some of the low
foothills of the Alps, and the channel of the River Adige in the
foreground. |
 |
View to the north from the tower |
A beautiful town! |
 |
The
Piazza della Erbe from the tower |
I ate lunch under
one of those umbrellas. If the plaza seems uncrowded, it is only
because it was very hot in the sun, and everyone was hiding in the
shade! |
 |
The
view to the southwest |
The Roman Era
arena is visible nearby. |
 |
The
Arena di Verona |
Built in the 1st
Century AD, the arena is the third largest still in existence. The
wall on the left is a remnant of the highest rim. The inner portion
is still used for performances today, seating as many as 25,000
people. Microphones are not necessary for the opera performances;
the acoustics are perfect. |
 |
WWII Holocaust Memorial |
In a park in the
Piazza Bra, we came across a memorial to Holocaust victims... |
|
|
|
|