Thursday, September 18, 2008

Today is the day we drove from Sciacca leaving Verdetechnica to get to our next destination in Alpecucco. Before setting off to Alpecucco, we spent the morning at Eraclea Minoa to look at an outcrop of Lower Gypsum.

The outcrop was full of branching selenite and gypsarenite. Once we all had a good look at the outcrop we had free time on the beach. Some swam, others bathed in the sun, and the professors enjoyed espressos at the beachside cafe. We had our lunch next to the vans while attempting to avoid the bees (they found us anyway) and then we were off for the long drive to Alpecucco.


On the way, we had a few stops looking at the basic tectonics in Central Sicily and the Corleone Formation. Central Sicily is made up of a complex fold and thrust system. The Corleone Formation is a rich in glauconite sandstone that is associated with the Nummidian Flysch.



There were a lot of sleepers on the way to Alpecucco.



We finally reached Alpecucco. It's a cute agritourismo and the rooms were nice. It's too bad we were only staying for one night.


Once we all unpacked and settled in we all waited for our guest lecturer for the night. Dr. Raimondo Catalano a professor at Palermo Univeristy in the mythical city of Palermo. He gave us an introduction on the geologic structure and stratigraphy of Central Sicily.


We had a late dinner which consisted of multiple courses once again but everything was delicious. As most of us turned in for the nights, other decided they needed some unwinding after a long day in the car. We decided to have a headlamp disco in the boys bunk.


Wednesday, September 17, 2008

Sept 17: Did someone say gypsum?

Sutera, Sicily


There was lots of driving today- Andy and Sanjoy were heroic!
Did we mention lots of turning around as well?


After inspecting tightly folded Lower Gypsum road cuts in the early morning, we found ourselves tightly folded in the narrow streets of Raffadali. We’re pretty certain that by the time we left, everyone knew we were there. Between working all morning on the road leading into town, parking in a spot too small for us at the main square, trooping 17 people into one small cafĂ© for coffee and pastries, driving the wrong way around the main square (dead ended at a 3 ft wall), squeezing down a road only a few centimeters wider than the big van, then accidentally blocking the main road while two of us ran into the bakery for lunch bread… Well, it was no surprise to learn that the whole area knew we were around, and was keeping an eye out for us.












Next we stopped at the remarkable Monte Banco, where all 10 sections of the Messinian Lower Gypsum unit can be seen. The block mountain is also set in a beautiful valley, so it was no trouble at all to follow Dr. Lugli on a tour of the sections on a nearby slope.

Afternoon brought lunch in Piazza di San Carlos in nearby Santa Elizabetta, a quiet village with some youths all too eager to show their scooter wheelies to us. Wear your helmets, kids!














The day finished in Sutera, a town situated high above the valley under a huge gypsum block. (Still the Lower Gypsum unit!) Unfortunately, once the professors mentioned fish fossils in a nearby diatomite section, we were lost for the day digging into the slope for our own. Congratulations to Rachel for finding the first one! Others found more fish, tree parts, leaves, and mud clasts.

After this, we were ready to dive into bed.

Tuesday, September 16, 2008

Mashed up gypsum

Today we looked at several other gypsum outcrops. This gypsum was different because it had been transported in large underwater flows called turbidites. In some places large gypsum crystals had grown into beautiful disks and "roses" in the rocks when they were still mud. Then the rocks were buried and heated turning the gypsum into alabaster.

In one field locality a slow landslide was causing the road to crack and slump leaving impressive deformation in a few years time.

Today we were home for lunch as reports are due tomorrow and we needed some time to get work done.

Monday, September 15, 2008

8 courses, 3 hours

1) Pasta

2) Fish
3)Salad
4)Fruit cup - missing photo
5) Pistachio cake

6)Ice cream
7) Espresso
8) Digestive

Sicily’s marvelous hospitality

Today, we set off for our “half-day” of work to the Italkali Salt Mine in Realmonte. The drive itself was wonderful, as yesterday’s rain cleared the sky, leaving Sicily free to invite us to some even more majestic scenery. The windy roads, smoking lorries, shady Sicilian overtaking manoeuvers and croaking walky-talkies added to the serene drive to the salt mine. Once there, the grandeur of the mine was striking only by its large entrance, big enough for semi-trucks to drive in. We buckled up and followed our miner-guides down the tunnel with our vehicles. We had to leave John Pohl’s car at the mine parking lot, since for flammability reasons, only diesel engines are allowed down the mine. We drove down for ~1 km, ending up in a very large “salt hall”. Yes, salt. While I knew I was in a salt mine, I was not expecting that the entire mine was drilled through salt. Salt Everywhere! Ceiling, walls, floor everything was salt! The dip (tilt) of the depositional beddings were very apparent by the darker (but very thin) clay layers that draped the beds back in the days (5+ million years ago), when those beds were the surface of the Earth. In this gigantic hall, an altar and ecclesiastical engravings were carved in the salt!

After spending some time our nose stuck to the walls, noticing how the grain sizes changed in different beds, and finding a dessication surface (like the cracked surface of dried mud, but salt instead), we hopped back into vans and drove further down the mine, ending up 75 meters below sea-level, and 200 meters below the surface. At these depth, salt, looses some of its mechanical strength and starts to flow because of the overburden pressure. As a result, we observed absolutely stunning folds in the salt layers, the different colors of the layers being due to their different compositions. While most of the layers were halite (“regular” salt) and white, other thinner ones were kainite (a complex salt containing magnesium and potassium) and yellow, while the thin brown ones were clay-rich. The wavelength of the folds were in fact related to the thicknesses of the layers! The thinner the layer, the more folds were present per unit distance. Then, the miners showed us a pile of salt (which were rock chunks, not like the powdery salt one buys in the supermarket), and we all went crazy! Nothing like a pile of rocks to distract geologists! After filling our packs and vans with samples, we returned to the vans and drove off, out of the mine.

We had two hours to kill before our lunch, soo… of the “Lido del sabbia d’oro”, or “the beach of the golden sand”! After negotiating some tight turns in this charming locality, some of us went to explore the lower gypsum unit exposed down the beach, while others took this opportunity to relax a little or take a swim in the sea, which had fun waves due to yesterday’s windy day. 15 minutes before 1pm, we started de-sanding ourselves, and headed to the beach-front restaurant. What a meal! Goodness, none of us expected such amazing food, particularly enhanced by the director of the mine, who treated us to 3 deserts, coffee and some liqueur!), but let’s backtrack a little… The restaurant outdoor tables are located on a wooden platform, under a tent, to protect us from the blazing sun, but with most of the sides open to allow a beautiful view of the beach and the sea. After downing several bottles of water, our first dish arrived and consisted of succulent shrimp-pasta with shrimp-and-lobster sauce, with pistachio “sprinkles”. Of course, this is only the antipasti, the main meal is yet to come, although several of us could not resist getting seconds on that pasta.. The main meal was a full fish, a dorade, cooked with tomatoes and other delicious herbs, served on a plate and aluminum foil. The result was a light and tender fish, accompanied wonderfully with local white wine. Dessert was a small fruit bowl, but then the generosity of our Sicilan hosts was made apparent when a second desert appeared in front of us, a layered cake with ricotta cheese in the middle. Delicious and stuffing! But suddenly, a third desert (!) was distributed! A “semi-freddo”, or “half-cold” ice-cream. Some of us had vanilla, others coffee. Feeling semi-comatose, a good meal in Sicily cannot be ended without the timeless espresso. Ahhh this frothy nectar of the gods was more than welcome, but who knew more was to come! A “spicy jaegger” liqueur called Amaro body-slammed the taste-buds one last time. This food extravaganza lasted 3 hours, ahhhh Sicily ☺

The mine director, who payed for the desserts, coffee and liqueur, then drove us to a site where apparently large gypsum (“gesso” in Italian) crystals lay in selenite (coarse-grained gypsum beds). We Indiana Jones’ed our way to the outcrop and did find some spectacular crystals (but secondary, thus not representing the crystals at the original time of deposition). We got back to “Verdetechnica”, our Agriturismo in Sciacca at almost 5pm; so much for our half-a-day work schedule! But what a day, and what a perfect example of how hospitable Sicily is!

Saturday, September 13, 2008

Many new additions

We started our day of geology today at a pleasant spot on the beach! We looked at the Trubi Formation - the rock formation above the upper and lower gypsum layers we visited earlier. We measured and described a section of this formation, which is composed of rhythmic beds of limestone and marls.















After working for the morning at the beach, we drove to a roadside outcrop to unravel a geological mystery! Here we saw a section of upper gypsum that was tilted vertically. In this section, two different gypsum beds on either side of a clay bed showed opposite directions were up! Only after close examination could we see evidence of folding that had deformed the layer - both directions really were up! The section had been tightly folded into an s-fold or z-fold structure. In this situation, the crystal growth habit was our best indicator of the original orientation of the beds.

Then we were off to find the Turkish Steps! This amazing formation sits right on the water, and is bright white. It actually looks like a gigantic set of steps down to the sea from the bluff above.



Today was a planned short day so we took a much-needed break and swam for about an hour here. After that we came back to Verdetechnica and worked on our assignments... good times!
















We finished the day with a delicious dinner of roasted chicken with sun-dried tomatoes and olives over rice, and a caprese salad. Ahhh, Sicily :)


Ciao!

Friday, September 12, 2008

More Gypsum


After the quarry we headed up the hill to a monument to Girabaldi, marking the location his first battle toward the unification of Italy.

In the afternoon we headed to Eraclea Minoa. In the morning, in Calatafimi, we had looked at the Lower Gypsum from the early Messinian. This afternoon, we looked at the Upper Gypsum from the late Messinian. More gypsum but vey different. In Eraclea Minoa, the crystals are vey long.

After our work was done we took a swim at the near by beach.