Titlebook: Landscapes and Landforms of Portugal; Gon?alo Vieira,José Luís Zêzere,Carla Mora Book 2020 Springer Nature Switzerland AG 2020 Geodiversit

閃光東本

The Tróia Peninsula—An Aeolian Sedimentological Legacyevolution of the most prominent Portuguese sand spit—the Tróia Peninsula. Data suggests that the spit has formed from Grimaldian dunes converted into barrier islands during the Holocene transgression, and coalesced by the accumulation of sediments transported by the northbound longshore drift. The T

Conquest

The Southwest Coast of Portugalts complex geomorphological evolution reflects the geostructural position near the contact of the African plate and the Iberian microplate, and the relative sea-level changes and characteristics of the coastal systems. The major landform of the region is the Littoral Platform, tilted to the northwes

DUST

寬度

The Granite and Glacial Landscapes of the Peneda-Gerês National Parkd in 1971 and it is the only national park and most important protected area in Portugal. The aesthetic attractiveness is supported mainly by the distinct granite landscape of the Gerês and Peneda Mountains, where the post-orogenic Variscan Gerês granite facies occurs. The rugged relief is poorly co

Enteropathic

PANIC

秘密會(huì)議

The Longroiva and Vilari?a Depressions: Two Narrow Tectonic Basins with Different Impacts on the Humke-slip fault, one of the largest tectonic structures in Portugal. The area has been focus of interest of geological and geomorphological research for several decades, mainly due to their rich heritage of Paleogene to Quaternary deposits that contribute to a better understanding of the regional evol

Dendritic-Cells

The Mondego River and Its Valleyf Figueira da Foz, it has a semi-torrential regime with irregular inter- and intra-annual discharge variations as a result of a Mediterranean climate. This regime was responsible for the occurrence of large floods, mainly in the Lower Mondego, a region that through history has also suffered from sig

CHASM

Ballerina