Geoheritage of the Iconic EN280 Leba Road (Huila Plateau, Southwestern Angola): Inventory, Geological Characterization and Quantitative Assessment for Outdoor Educational Activities

Autor: Fernando Carlos Lopes, Anabela Martins Ramos, Pedro Miguel Callapez, Pedro Santarém Andrade, Luís Vítor Duarte

Publikováno v: Land, Vol 13, Iss 8, p 1293 (2024)

The EN280 Leba Road is a mountain road that runs along the western slope of Serra da Leba (Humpata Plateau) and its outstanding escarpments, connecting the hinterland areas of the Province of Huila to the coastal Atlantic Province of Namibe, in South

Externí odkaz: https://doaj.org/article/0a0c724b42544812a1eb5e34d825541c

Mechanisms and age estimates of continental-scale endorheic to exorheic drainage transition:Douro River, Western Iberia

Autor: Gerardo de Vicente, António A. Martins, Jan-Pieter Buylaert, João Cabral, Fernando Carlos Lopes, Loreto Antón, Alberto Gomes, Martin Stokes, Andrew S. Murray, Pedro P. Cunha, Diamantino Insua Pereira

Publikováno v: Cunha, P P, Martins, A A, Gomes, A, Stokes, M, Cabral, J, Lopes, F C, Pereira, D, de Vicente, G, Buylaert, J P, Murray, A S & Antón, L 2019, ' Mechanisms and age estimates of continental-scale endorheic to exorheic drainage transition : Douro River, Western Iberia ', Global and Planetary Change, vol. 181, 102985 . https://doi.org/10.1016/j.gloplacha.2019.102985
Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos)
Agência para a Sociedade do Conhecimento (UMIC)-FCT-Sociedade da Informação
instacron:RCAAP
Repositório Científico de Acesso Aberto de Portugal
Repositório Científico de Acesso Aberto de Portugal (RCAAP)

In western Iberia, mechanisms that can explain the transition from endorheic to exorheic continental-scale drainage reorganization are foreland basin overspill, headwards erosion and capture by an Atlantic river, or a combination of both. To explore

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::ba6f238519bf148efdf377ab21fcb080
https://pure.au.dk/portal/da/publications/mechanisms-and-age-estimates-of-continentalscale-endorheic-to-exorheic-drainage-transition(276001be-ee5b-4b93-bdb6-34b34f52dd27).html

Paisagens da Islândia: Formas e Processos (III)

Autor: Fernando Carlos Lopes

Publikováno v: Revista de Ciência Elementar. 6

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::3083493dc04ff18b2bde5d1167b88ad0
https://doi.org/10.24927/rce2018.048

The development of the Deception Island volcano caldera under control of the Bransfield Basin sinistral strike-slip tectonic regime (NW Antarctica)

Autor: Fernando Carlos Lopes, Adriane Machado, M. T. Barata, A. T. Caselli

Publikováno v: Repositório Científico de Acesso Aberto de Portugal
Repositório Científico de Acesso Aberto de Portugal (RCAAP)
instacron:RCAAP

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::47396b4383eb3fea248c153e83046168
https://doi.org/10.1144/sp401.6

The River Mondego terraces at the Figueira da Foz coastal area (western central Portugal): Geomorphological and sedimentological characterization of a terrace staircase affected by differential uplift and glacio-eustasy

Autor: Lúcio Cunha, Andrew S. Murray, Alberto Gomes, Fernando Carlos Lopes, Jan-Pieter Buylaert, Pedro P. Cunha, Anabela Ramos

Publikováno v: Ramos, A M, Cunha, P P, Cunha, L S, Gomes, A, Lopez, F C, Buylaert, J-P & Murray, A S 2012, ' The River Mondego terraces at the Figueira da Foz coastal area (western central Portugal) : Geomorphological and sedimentological characterization of a terrace staircase affected by differential uplift and glacio-eustasy ', Geomorphology, vol. 165-166, no. Special issue, pp. 107-123 . https://doi.org/10.1016/j.geomorph.2012.03.037
Repositório Científico de Acesso Aberto de Portugal
Repositório Científico de Acesso Aberto de Portugal (RCAAP)
instacron:RCAAP

A geomorphological and sedimentological characterization of the River Mondego terraces in the Figueira da Foz coastal area, Portugal, is presented. The relief is dominated by a Pliocene a marine sandy unit ~10–15 m thick, reaching ~250 m a.s.l., th

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::820990cfa8d290521b7df5516277e8e9
https://doi.org/10.1016/j.geomorph.2012.03.037