Mediterranean pilot.

v. 3. The southeast of Italy, the shores of the Adriatic and Ionian Seas to Cape Matapan -- v. 4. From Cape Matapan (Greece) eastward, the Mediterranean archepelago, and the southern shore of the Mediterranean Sea, eastward to Ras Asjdir(Libia).

Hedwig Beaker, front

5 33/64 in.x 5 33/64 in.; wheel-cut glass

Hedwig Beaker, full front

5 33/64 in.x 5 33/64 in.; wheel-cut glass

National tales /

v. 1 The Spanish tragedy. The miracle of the holy hermit. The widow of Galicia. The golden cup and the dish of silver. The tragedy of Seville. The lady in love with romance. The eighth sleeper of Ephesus. Madeline. Masetto and his mare. The story of Michel Argenti. The three jewels. Geronimo and Ghisola. The fall of the leaf. Baranga.--v. 2 The exile. The owl. The German knight. The Florentine kinsmen. The carrier's wife. The two faithful lovers of Sicily. The Venetan countess. A tale of the harem. The chestnut tree. The fair maid of Ludgate. The three brothers.

Legge, decreti, e regolamenti per la organizzazione, ed attribuzioni della Gran corte de'conti in Sicilia.

Mode of access: Internet.

Restitution du temple d'Empédocle à Sélinonte; ou, L'architecture polychrôme chez les Grecs.

Mode of access: Internet.

Memorie degli scrittori cosentini /

Reprint of the 1750 ed. published by Stamperia de' Muzj, Naples.

Italy, handbook for travellers,

Each part also issued separately.

Italy : handbook for travellers /

"Index of streets and plans of Rome": v. 2, 18 p. at end.

Italy : handbook for travellers /

pt. 1. Northern Italy, including Leghorn, Florence, Ravenna, the Island of Corsica, and routes through France, Switzerland, and Austria. 8th remodelled ed. 1889. -- pt. 2. Central Italy and Rome. 10 rev. ed. 1890. -- pt. 3. Southern Italy and Sicily, with excursions to the Lipari Islands, Malta, Sardinia, Tunis, and Corfu. 10 rev. ed. 1890.

Italy; handbook for travellers,

Pt. 2-3: 13th rev. ed.

The lost tales of Miletus.

Advertisements on p. 1-8 at end.

Die Baukunst in Sizilien. die griechische, römische, byzantinische, arabische und normannische Baukunst : sowie der Entwurf eines groszstädtischen Volks- und Luxusbades in modernisiert arabisch-normannischer Bauweise /

No more published after I. Teil.

On the Mediterranean conveyor belt system

The Mediterranean Sea is a semi-enclosed sea, connected to the Atlantic Ocean through the Gibraltar Strait and subdivided in two different regions by the Sicily Strait. The geographical extension of the basin, the surface heat flux, and the water inflow from the Gibraltar Strait are some of the basic factors determining its horizontal and vertical circulation. In the Mediterranean strong salinity and temperature zonal gradients contribute to maintain the zonal-vertical circulation, while meridional-vertical cells are equally forced by winds and deep water mass formation in three regions, the Gulf of Lyon, the southern Adriatic and the Cretan Sea areas. The objective of this thesis is to study how these cells combine together to form the Mediterranean conveyor belt system. This has never been attempted before so the conclusions are necessarily preliminary. In the first part we discuss the vertical zonal and meridional circulation by reconstructing the Wust Mediterranean vertical salinity and temperature structures in an attempt to evaluate the water mass structure consistent with modern data. Our results confirm that Wust depicted vertical circulation from scarce data is reproduced by the past 27 years observations. The structure of both meridional and zonal circulations was discussed using velocity vertical streamfunctions with two different methods. The first one, eulerian, allowed us to observe vertical structures that were already reported in the literature. Recent studies in the Atlantic Ocean have shown that gyres and eddies have an important influence in the isopycnal vertical circulation. This is called the residual circulation which was computed in this study for the first time. A possible interpretation of horizontal connection between the meridional and zonal cells was discussed using horizontal streamfunction. In the last part of the thesis we have been developing an idealized numerical model to study the vertical circulation in the Mediterranean.

(Table 3) Mediterranean core-top d18O values for various planktonic foraminiferal species

A box model is presented to simulate changes in Mediterranean long-term average salinity and d18O over the past 20,000 years. Simulations are validated by comparison with observations. Sensitivity tests illustrate robustness with respect to the main assumptions and uncertainties. The results show that relative humidity over the Mediterranean remained relatively constant around 70%, apparently narrowly constrained to the lower end of the range observed globally over sea surfaces by the basin's land-locked character. Isotopic depletion in run off, relative to the present, is identified as the main potential cause of depletions in the Mediterranean d18O record. Also, slight increases in relative humidity (of the order of 5%) might have caused very pronounced isotopic depletions, such as that in sapropel S5 of the penultimate interglacial maximum. The model shows distinctly non proportional responses of d18O and salinity to environmental change, which argues against the use of isotope residuals in Mediterranean paleosalinity reconstructions.