Ptolemy's Tetrabiblos, or Quadripartite: being four books of the influence of the stars.

Plate wanting.

Le nord de l'Afrique dans l'antiquité grecquë et romaine, étude historique et géographique ... accompagné de quatre cartes,

Mode of access: Internet.

Ueber die Einwohner Deutschlands im II. Jahrhundert der christlichen Zeitrechnung, namentlich über Sachsen und Bayern nach Claudius Ptolemaeus ... /

Includes quotations in Latin.

Astronomische untersuchungen über die mondfinsternisse des Almagest ...

Mode of access: Internet.

Lettre à Flora.

Greek text and French translation of: Pros Phlōran.

Holocene tsunami events in the Eastern Ionian Sea - Geoscientific evidence from Cefalonia and the western Peloponnese (Greece)

This study presents geo-scientific evidence for Holocene tsunami impact along the shores of the Eastern Ionian Sea. Cefalonia Island, the Gulf of Kyparissia and the Gialova Lagoon were subject of detailed geo-scientific investigations. It is well known that the coasts of the eastern Mediterranean were hit by the destructive influence of tsunamis in the past. The seismically highly active Hellenic Trench is considered as the most significant tsunami source in the Eastern Ionian Sea. This study focuses on the reconstruction and detection of sedimentary signatures of palaeotsunami events and their influence on the Holocene palaeogeographical evolution. The results of fine grained near coast geo-archives are discussed and interpreted in detail to differentiate between tsunami, storm and sea level highstands as sedimentation processes.rnA multi-method approach was applied using geomorphological, sedimentological, geochemical, geophysical and microfaunal analyses to detect Holocene tsunamigenic impact. Chronological data were based on radiocarbondatings and archaeological age estimations to reconstruct local geo-chronostratigraphies and to correlate them on supra-regional scales.rnDistinct sedimentary signatures of 5 generations of tsunami impact were found along the coasts of Cefalonia in the Livadi coastal plain. The results show that the overall coastal evolution was influenced by tsunamigenic impact that occured around 5700 cal BC (I), 4250 cal BC (II), at the beginning of the 2nd millennium cal BC (III), in the 1st millennium cal BC (IV) and posterior to 780 cal AD (V). Sea level reconstructions and the palaeogeographical evolution show that the local Holocene sea level has never been higher than at present.rnAt the former Mouria Lagoon along the Gulf of Kyparissia almost four allochtonous layers of tsunamigenic origin were identified. The stratigraphical record and palaeogeographical reconstructions show that major environmental coastal changes were linked to these extreme events. At the southern end of the Agoulenitsa Lagoon at modern Kato Samikon high-energy traces were found more than 2 km inland and upt ot 9 m above present sea level. The geo-chronological framework deciphered tsunami landfall for the 5th millennium cal BC (I), mid to late 2nd mill. BC (II), Roman times (1st cent. BC to early 4th cent. AD) (III) and most possible one of the historically well-known 365 AD or 521/551 AD tsunamis (IV).rnCoarse-grained allochthonous sediments of marine origin were found intersecting muddy deposits of the quisecent sediments of the Gialova Lagoon on the southwestern Peloponnese. Radiocarbondatings suggest 6 generations of major tsunami impact. Tsunami generations were dated to around 3300 cal BC (I), around the end of 4th and the beginning of 3rd millennium BC (II), after around 1100 cal BC (III), after the 4th to 2nd cent. BC (IV), between the 8th and early 15th cent. AD (V) and between the mid 14th to beginning of 15th cent. AD (VI). Palaeogeographical and morphological characteristics in the environs of the Gialova Lagoon were controlled by high-energy influence.rnSedimentary findings in all study areas are in good accordance to traces of tsunami events found all over the Ionian Sea. The correlation of geo-chronological data fits very well to coastal Akarnania, the western Peloponnese and finding along the coasts of southern Italy and the Aegean. Supra-regional influence of tsunamigenic impact significant for the investigated sites. The palaeogeographical evolution and palaeo-geomorphological setting of the each study area was strongly affected by tsunamigenic impact.rnThe selected geo-archives represent extraordinary sediment traps for the reconstruction of Holocene coastal evolution. Our result therefore give new insight to the exceptional high tsunami risk in the eastern Mediterranean and emphasize the underestimation of the overall tsunami hazard.

Libri tres Ad autolycu. /

Greek text with Latin translation on opposite pages.

Apollonii Dyscoli qvae svpersvnt recensvervnt, apparatvm criticvm, commentarivm, indices adiecervnt Richardvs Schneider et Gvstavvs Vhlig.

vol. I. fasc. I. Apollonii scripta minora a Richardo Schneidero edita continens. 1878.--vol. I. fasc, II. Richardi Schneideri Commentarivm criticvm et exegeticvm in Apollonii scripta minora continens. 1902.--vol. II. Apollonii Dyscoli De constrvctione libri quattvor recensvit apparatv critico et explanationibvs instrvxit Gvstavvs Vhlig. Adiectae svnt tabvlae phototypicae dvae. 1910.--vol. III. Praefationem ediecit, librorvm Apollinii deperditorvm fragmenta collegit, disposuit, explicavit, indices omnivm librorvm confecit Richardvs Schneider. 1910.

Oppianou Kynēgētika kai Halieutika. Oppiani Cynegetica et Halieutica,

Latin translation by David Peifer.

Corpvs apologetarvm christianorvm saecvli secvndi

Vols. 3-5 have imprint: Ienae, svmptibvs G. Fischer (olim F. Mavke); v. 6-8: Ienae, apud F. Mauke; v. 9: in libraria Maukii (H. Dufft)

Festival at Meron.

Mode of access: Internet.

Observationes ad S. Pompeii Festi Paulique excerpta.

Pr.

Epitomē tēs Katholikēs prosōdias Hērōdianou /

Includes index.

Moeridis Atticistae Lexicon atticum cum Jo. Hudsoni, Steph. Bergleri, Claud. Sallierii, aliorumque notis.

Mode of access: Internet.

M. Verrii Flacci quae extant et Sexti Pompeii Festi de verborum significatione, libre XX /

"Index in Festi fragmentum et schedas": v. 2, p.xxix-xxxix.