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Syriac as evidence for Greek Monastic Florilegia

Review of Fundamentals of New Testament Greek

Local initiatives and their chances to drive socioecological change: Social cooperatives on the Greek island of Samothraki

Review of Advances in the Study of Greek : New Insights for Reading the New Testament

More than Scapegoating : the Therapeutic Potential of Stories of Child-killing demons in Ancient Greece and Rome

‘Pirates’ in EU’s (Semi)Peripheries: A Comparative Case Study on the Perceptions of Poles and Greeks on Digital File-sharing

Tormented by History: Nationalism in Greece and Turkey

Beyond the Intractability of the Greek-Macedonian Dispute

A rational-actor perspective on the origin of liturgies in ancient Greece

Some Bibliographic Notes on Greek New Testament Manuscripts

An introduction to ancient Greece. The Aegean and its neighbors c. 7000-700 B.C.

An Introduction to Ancient Greece. The Aegean and its Neighbors c. 7000-700 B.C.

Abstract is not available.

'Colonising' the past: history and memory in Greece and Turkey

Institutional change and economic performance in Greece

Contested Geographies: Greece, Turkey and the Territorial Imagination

Review of The Textual History of the Greek New Testament: Changing Views in Contemporary Research

Review of Verbal Aspect Theory and the Prohibitions in the Greek New Testament

Translation and standardisation into Greek of the standardised general Nordic questionnaire for the musculoskeletal symptoms

Flora and vegetation of Andros, Kikladhes, Greece.

An annotated list of the known vascular plants of Andros is provided, with notes on ecological preferences, altitudinal distributions and frequency. The total number of native and naturalized taxa of vascular plants listed is 1055. Exact localities are provided for the rarest species on the island. 74 maps are also provided for species with variously delimited distribution. For the species known t

The pre-fysch and basal shaly flysch deposition in the Parnassus-Ghiona Zone, central Greece

The interruption in deposition during the K/T transition in the Parnassus-Ghiona Zone caused the formation of hardgrounds and intraformational conglomerates in the central parts. During the later part of the early Paleocene to the middle or early part of the late Paleocene a shallow sea covered central Parnassus; stromatolites formed in broad valleys and phosphatic calcarenitic accumulations in sm