闪光东本 发表于 2025-3-25 05:48:48
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 TConquest 发表于 2025-3-25 07:44:52
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 northwesDUST 发表于 2025-3-25 12:31:43
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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 coEnteropathic 发表于 2025-3-25 21:48:20
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The Longroiva and Vilariça 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 evolDendritic-Cells 发表于 2025-3-26 08:52:06
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 sigCHASM 发表于 2025-3-26 14:33:29
http://reply.papertrans.cn/59/5808/580752/580752_29.pngBallerina 发表于 2025-3-26 20:38:28
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