COMPARATIVE ECONOMETRIC ANALYSIS ON THE EVOLUTION OF TOURISM TRAFFIC IN PRAHOVA AND BRASOV COUNTIES
The paper analyzes the comparative development of tourist traffic in the counties of Prahova and Brasov, the main indicators for assessing values, numbers of tourist arrivals and overnights number, being studied as econometric time series. The economic crisis triggered worldwide began before 2009 also in travel industry, has important effects at national level in Romania territorial. Studied in this context is the tendency of tourist movement in Prahova and Brasov counties, and recording developments oscillatory growing up in 2008 and a significant decrease in the year 2009. Conclusions of the analyzed phenomena show that the results are the effects of the emergence of financial bottlenecks that led to a significant drop in income population and therefore in important reduction of the tourist arrivals and of the overnight stays in these counties. However, it is expected a revival of tourist traffic in Prahova and Brasov counties, after economic recovery of Romania.
Analysis of the correlation between the existing accommodation capacity and the number of tourists arrived in Suceava County structures of touristic reception.
In the international touristic practice, but also in the specialized literature, it is perceived the population’s trend to spend the leisure time in an active way, by practicing tourism. It is also noted the fact that the forms of tourism organized in the big crowded centers, with fixed, rigid, monotonous programs, with journeys from a crowded environment to another, don’t satisfy anymore the tourists’ aspirations, motivations, options. They prefer the countryside zones that offer a non-polluted environment, with a natural and cultural potential very slightly altered. Such an area, which is inscribed in the rich heritage of the Romanian tourism, is Suceava County, which, by its offer, may be envisaged as an exceptional touristic zone of Romania. Suceava County, Bârsa Land’s progress demands the inclusion of the principals of the lasting regional development in its development strategy. Within this framework, the importance of studying and analyzing the touristic activity’s evolution can be noted. The need of acknowledging the fluctuations registered by the results of the touristic activity deployment allowed the approach of the issue related to the correlation stage between the existing accommodation capacity and the number of tourists arrived in the accommodation structures of Suceava County during the 2000-2006 period. The mutual involvement relationship, the existence, the direction, the form and the intensity of the connection between the two indicators are analyzed in this paper. The conclusions stated following the analysis of the obtained result, represent an upper step for filling in the image regarding the regional tourism activity in the conditions of the establishment and application of certain regional lasting development strategies.
Mesozoic rifting and basin inversion along the northern African Tethyan margin: an overview
Abstract The northern African Tethyan margin registered three major rifting episodes from the latest Palaeozoic-earliest Mesozoic to the earliest Cenozoic. Break-up of Gondwana was initiated in the late Carboniferous. Along the northern African-Arabian plate margin rifting propagated westward from the northeastern Arabian margin to Morocco during the Permian and Triassic, and was accompanied by Mid-Late Triassic-earliest Liassic extensive alkaline flow basalts. Rifting continued during the Liassic, e.g. in the Moghrebian Atlas troughs. A second stage of rifting occurred in the Late Jurassic and continued into, or was rejuvenated during, the Early Cretaceous. Along the east Mediterranean margin, some large E-W trending rifts formed, often with associated volcanism, e.g. southern Sirt and Abu Gharadig. Most researchers believe the oceanization of the eastern Mediterranean basin occurred at this time. Flexural subsidence affected the Moghrebian Atlas, including the Riffian-Tellian domain, where a thick flysch series was deposited. Two short-lived, but widespread and tectonically important, compressional or wrench-dominated events occurred during the Santonian and the latest Maastrichtian. From Morocco to Oman, most sedimentary basins were folded and inverted at these times. The Santonian event resulted from onset of the collision between the African-Arabian and Eurasian plates. New stress-fields favoured NE-SW extension along the African plate margin, generating or rejuvenating some rifts, e.g. in the Euphrates trough and in the Libya-Tunisia region (northwestern Sirt, Pelagian Sea). Rifting and magmatism continued in these regions into the Paleocene. During the Mesozoic, therefore, the northern margin of the African-Arabian plate registered both rifting resulting in the oceanization of the Tethys and rifting resulting from the initiation of the closure of the Tethys. The intraplate domain exhibited echoes of the tectonic events affecting the margin.