Wyniki wyszukiwania - BazTech

Ograniczanie wyników

Znaleziono wyników: 2

Liczba wyników na stronie

Wyniki wyszukiwania

Wyszukiwano:
w słowach kluczowych: Albanian Alps

Sortuj według:

Ogranicz wyniki do:

Environmental Landscapes in the "Albanian Alps" in Kosovo in the Development of Local Tourism

Hasanaj Petrit, Kuqi Bekë

Ecological Engineering & Environmental Technology

2022

Vol. 23, iss. 6

188--194

The positioning of the Albanian Alps region as part of the Balkan Alps and the landscape values it carries are some of the main elements that have influenced the formulation of strategic orientations. At the same time, the region of the Albanian Alps will differ from the rest across the border in terms of themes, types of tourism, offer, activities, cultural heritage, history, etc. Regardless of the quality of the physical connections, this territory with its dynamics plays an important role in the region, transforming into a "connecting bridge" between Kosovo and Montenegro. In this area, tourism is focused on the creation of independent accommodations with sleeping and breakfast, where visitors will have the opportunity to be in contact with the residents, with the lifestyle of the community and with the local cuisine. The typical accommodation offer in this area consists of private and semi-private accommodation in which the owner provides services, including the preparation of local food. The most attractive whole is made up of forests, grasslands, meadows, rivers and ravines, steep hills and lakes that complete the features of the landscape and provide a pleasant experience of this nature with high attractive tourist values. Also, the high mountain and rocky massifs offer the possibility of mountaineering.

The Permian and Triassic in the Albanian Alps

Gaetani M., Meço S., Rettori R., Henderson C. M., Tulone A.

Acta Geologica Polonica

2015

Vol. 65, no. 3

271--295

The sedimentary succession of the Permian to Middle Triassic of the Albanian Alps is described, as part of the eastern Adria passive margin towards the Tethys. A carbonate ramp deepening towards NE in present day coordinates developed during the Middle Permian and was affected by block faulting with the deposition of carbonate breccia. The Early Triassic was characterized by intense terrigenous deposition with several cobble conglomerate units up to 80 m-thick, and by oolitic carbonate shoals. The fine clastic deposition ended gradually during the earliest Anisian and a wide calcarenitic ramp occupied the area, with small local carbonate mounds. Basinward, the red nodular limestone of the Han Bulog Formation was interbedded with calcarenitic material exported from the ramp. Drowning to more open conditions occurred towards the end of the Pelsonian. Subsequently, cherty limestone and tuffitic layers spread over the entire area. Towards the end of the Ladinian, with the end of the volcanic activity, red pelagic limestone was deposited locally for a short period. By the latest Ladinian most of the area returned to shallow-water conditions, with a peritidal carbonate platform. In the Theth area, in contrast, a basin with black organic-rich dolostone and limestone developed which seems to be unique in that part of the Adria passive margin. The occurrence of cobble conglomerate units in the Lower Triassic testifies to very active block faulting and high accommodation, not yet described for the area.