Mark Wilson June 8th, 2013
MILAZZO, SICILY, ITALY–The pre-conference field trip of the International Bryozoology Association has now almost completely circled Sicily. We are in the far northeastern corner of the island on a rocky cape jutting into the sea towards mainland Italy. The drive here along the very steep and rocky north coast of Sicily was fantastic, especially the seaward views of the volcanic Aeolian Islands (including the famous Stromboli).
Our day started on the furthest western part of Sicily. We took a short boat trip into the Stagnone di Marsala lagoon to the ruins of the ancient Phoenician walled city Mozia. The top photo is a view of the silted-up south harbor of the island with remnants of its guard towers on either side of the narrow entrance. Mozia was settled in the 8th Century BCE as a commerce center. It was well-suited to the Phoenician way of life with its small but safe ports and a defensible interior. The island is in the middle of an extensive lagoon which protects it from the ravages of the open sea (and invaders — for awhile). The site is still being actively excavated and studied.
There is a collection of terra cotta masks in the museum of apparently ceremonial use. This one seems delightful until you learn tat one of those ceremonies was human sacrifice, primarily of children. Now this character looks far more sinister.
Greeks under the tyrant Dionysius captured the island and is city after a siege in 397 BCE. The fall of Mozia is recorded subtly by remnants of literally last ditch earthworks and fires. The stones of this guardhouse along the wall on the southern coast were reddened when the associated wooden structures were burned either during or just after the siege.
The Stagnone di Marsala lagoon was formed during the Pleistocene as an abraded marine platform cut into fossiliferous marls and soft limestones. In this view from the island to the mainland you can see six whitish piles of salt on the distant shore. These are harvested from low ponds with walled enclosures (see below). The windmills, iconic for this area, pump water from one pond to another to control the mineral phases of the precipitates. This salt production goes back to antiquity.