This study focuses on potential athletic language in Phil 3:12-16. The main focus is the question what the assumption of the presence of athletic language in this text contributes to understanding it and especially its theological meaning better. The study consists of three parts. In part 1, the author analyses the preceding and the subsequent context of Phil 3:12-16 joining the defenders of a concentric structure: 3:1-11 (A), 3:12-16 (B), 3:17-4:1 (A’). The two framing sections (A and A’) focus on the opposition between Paul and his opponents, but the main point is Paul’s command to the Philippian addressees to “stand firm in the Lord”. Part 2 contains a brief exegetical analysis of 3:12-16. Our analysis focuses on the most important words (gaining/attaining; movement; thinking) and the goal of heavenly perfection with which they are connected. In the third part we analyse the potential athletic images in 3:12-16 which finds its “anchor point” in the noun τὸ βραβεῖον in 3:14. Based on the acceptance of this noun as an agonistic terminus technicus, other verbs and nouns which are not in and of themselves referring to athletics are interpreted as having an athletic meaning in our context. The study concludes with the caution that Paul counterbalances the “effort-reward scheme” of athletic language with the “giving-receiving scheme” of his call language. In this way, Paul introduces an emphasis on the future-orientedness of the message which is characteristic of his preaching and living.
The paper presents characteristics of the Pleistocene sediments in the western part of the Holy Cross Mountains. They are subdivided into four complexes and their stratigraphic setting is referred to the updated scheme for the Pleistocene of Poland. The Preglacial Complex includes fluvial sediments characteristic for its lack of Scandinavian material. Sediments of three main glaciations (Nidanian, Sanian 1 and Sanian 2) within the South Polish Complex, are referred also as the South Polish Glaciations. The oldest of these glaciations (Nidanian) is separated from the middle glaciation (Sanian 1) by sediments of the Podlasian Interglacial, represented by clay at the Kozi Grzbiet Cave that contains faunal remains and record of the Brunhes/Matuyama palaeomagnetic boundary. During the middle (Sanian 1) and youngest glaciation (Sanian 2), the Holy Cross Mountains were almost completely covered by the Scandinavian ice sheet, forming glacial deposits separated by fluvial series of the Ferdynandovian Interglacial. The Middle Polish Complex begins with sediments of the Mazovian Interglacial, represented by a pollen record from the Zakrucze site. They are followed by deposits of periglacial and fluvial origin of the Liwiecian Glaciation, Zbójnian Interglacial, Krznanian Glaciation and Lublinian Interglacial. The following glaciation (Odranian) is represented by the youngest glacial deposits that document presence of the Scandinavian ice-sheet in the westernmost part of the Holy Cross Mountains. The North Polish Complex is composed of a climatic warming (Eemian Interglacial) and cooling (Vistulian Glaciation), and is represented by valley and periglacial deposits. The last cooling of the Pleistocene is recorded in faunal remains in the Raj Cave.
Hot point drills were carried through in the Hans Glacier (Spitsbergen). For that purpose a non-cored hot point drill of 700 wattage was constructed. It was used among others for installing the ablation-movement stakes, for hydrological observations and in the boreholes an ice temperature was controlled.