The work is not a full-scale history of Rhodes in the Hellenistic age, the materials for which do not exist. It is rather an analysis of the ancient literary tradition regarding Hellenistic Rhodes on the one hand, and on the other an attempt to analyse, classify and exploit the very large body of epigraphical evidence in so far as it relates to the external aspects of Rhodian life. The results of this scrutiny of the epigraphical basis, here undertaken on a far wider basis than has ever before been possible, are as disappointing as conclusions based solely on epigraphical evidence are apt to be. The first half of the work examines in detail the tradition regarding the political history of Rhodes from 408/7 B.C., the year of the foundation of the city, to 164 B.C., the year in which Rhodes concluded an alliance with Rome, and thereby lost, largely in not wholly, the freedom of action which she had until then retained.

<p>The kinematics and associated deformation of upper crust in fossil and active convergent tectonic settings require different methods of study. In this thesis, I analyzed an example of a fossil convergent setting, the formation of the eastern portion of Paleoproterozoic Sudbury Basin, Ontario, and an example of an active convergent plate interface represented by the ongoing subduction along the Hellenic Arc at Rhodes, Greece. In Sudbury, using paleomagnetic remanence directions and Matachewan dyke orientations, I constrain the magnitudes of rotation associated with the formation of the NE-lobe, a tight secondary fold of the Sudbury Basin, as well as localize the fold axis and magnitude of rotation along the West Bay Anticline, a hitherto unknown fold of the Basin.</p> <p>For the Island of Rhodes, I corroborate the existence of two phases of Plio-Pleistocene or younger deformation including providing their principal strain axis orientations from a fault-slip analysis. In addition, I estimate the magnitude of slip from faults to generate respective incremental strain ellipses of the two deformation phases for the Island. The first phase is characterized by vertical shortening (ŝ₃) and N-S extension (ŝ₁) with associated normal faulting while the second phase is characterized by N-S shortening (ŝ₃) and E-W extension (ŝ₁) associated with strike-slip faulting.</p> / Master of Science (MSc)