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EN
The zones along the Baltic and the Adriatic have substantial geographical, economic and transport similarities. The strengthening of economic growth and the dynamics of the flow of goods has provided intermodality the utmost importance. The development of multimodal transport network and its connection with the TEN-T1 corridors represents a precondition for strengthening national economies. Baltic-Adriatic corridor connects the north and the south of Europe, with a more progressive intensification of the economic growth of Baltic and Central European countries. The intermodal transport system in the corridor has the ability to generate and intensify the economical-ly sustainable growth. Without doubt, there is a true need for economic growth and transport system within which intermodal transport would have particular significance as a strategic program. Strategic planning of transport development must be in the service for the overall economic growth and it should be dynamically adjusted to the objective investment possibilities in the field of intermodality.
PL
Strefy leżące na obszarze pomiędzy Bałtykiem i Adriatykiem charakteryzują się znaczącymi podobieństwami pod względem geograficznym, ekonomicznym i transportowym. Umacnianie wzrostu ekonomicznego oraz dynamiki przepływu dóbr zapewnia intermodalności najwyższe znaczenie. Rozwój sieci transport multi-modalnego i jego połączenie z korytarzami transportowymi TEN-T reprezentuje warunek wstępny dla umac-niania narodowych gospodarek. Korytarz Bałtyk-Adriatyk łączy południe i północ Europy, ze zwiększającą się intensyfikacją wzrostu gospodarczego w krajach środkowej Europy oraz krajach bałtyckich. System transportu intermodalnego w korytarzu daje możliwość generowania i nasilania utrzymywanego wzrostu ekonomicznego. Bez wątpienia, istnieje prawdziwa potrze-ba wzrostu ekonomicznego oraz tworzenia system transportowego, wewnątrz którego transport intermodalny miałby szczególne znaczenie, jako program strategiczny. Planowanie strategiczne celowane w rozwój transportu musi służyć ogólnemu wzrostowi gospodarczemu i powinno być dynamicznie dostosowane do możliwości inwestowania w obszarze intermodalności.
EN
The Adriatic Sea is an epicontinental, closed sea, part of the Mediterranean. It formed in the Late Miocene, and ended structurally during the Pliocene and Quaternary, when most of its sediments were deposited. The larger Pliocene and Quaternary depressions occur mostly by the western coast, where the deposits are several thousand metres thick, and were sourced from the Alps and the Apennines. The east coast is characterised by the large and elongated Dinarides Mts., that have continental drainage extremely close to the shoreline and a very small erosional rate. Consequently, eastern inflows were and are very short, including strongly tidal estuaries that erode only small volumes of mostly carbonate detritus, adjacent to frontal islands or mountains, with restricted depositional areas. The Neretva River deposits make up part of the largest contemporary delta system on the eastern Adriatic coast, and have been analysed in this study using three seismic sections and one exploration well. These deposits are recognized inside the Neretva and Korčula channels, assuming that processes operating during Quaternary glacial phases shifted the delta tens of kilometres to the west in the past on several occasions.
EN
The Central Europe Geodynamics Project (CERGOP) was initiated in 1993 [Fejes et al., 1993] and continued in 1995 as a European Union (EU) supported program. In 2003 the CERGOP-2/Environment Project, the successor of CERGOP, was commenced [Pesec, 2002]. The undertaken work in the CERGOP-2/Environment Project are shared and distributed to work packages. The work packages lO.x are formed to serve the main scientific users of the Central European GPS Geodynamic Reference Network (CEGRN) data. The work package 10.3 is devoted to integrate those geological and geophysical data that have primary importance regarding the present-day geodynamics of the Pannonian basin and its surroundings from the Adriatic microplate to the Carpathian Arc. This report is given about the works carried out between September 2003 and March 2004.
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