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Discover the ecotourism activities and boat trips we have available in Ria Formosa.Come visit this beautiful area and enjoy incredible moments during your holidays in the Algarve.Seismostratigraphic interpretation and isochron maps allowed for the establishment of the main oceanographic, climatic, morphologic and tectonic factors that controlled the drifts deposition: i) the Pliocene and Quaternary MOW circulation forced by climate changes; ii) the sea bottom topography inherited from the Late Miocene, mainly shaped by the Portimão, Lagos and Bartolomeu Dias canyons system; iii) the interaction between along-slope and down-slope processes since the Pliocene; and iv) Pliocene–Quaternary fault-activity and diapirism.► A new model for contourite drifts deposition off south Iberia since Early Pliocene.► Precursor, build up, growth phases identified due to time vs space geometric change.Its vestiges lie in the vicinity of the resort and marina of Vilamoura, in the civil parish of Quarteira, municipality of Loulé Municipality.during the 2nd century, the region of the Algarve fell under the domain of Rome, under the rule of Gaius Julius Caesar Augustus (23 September 63 BC – 19 August AD 14).Our tours and boat trips are available all year with several daily departures from Olhão and Faro.

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The seismostratigraphic interpretation of a dense array of oil industry seismic and stratigraphic correlation allowed the identification of five seismic units of Early Pliocene through Holocene in the Faro and Albufeira drifts and four correlative seismic units in the Lagos and Sagres drifts and three in the Portimão drift.

Surfing was the theme that inspired yet another Sketch Tour Portugal trip along the coast, taking advantage of the Rip Curl Pro event, one of the most important events in the international surfing calendar.

Many beaches, different waves, fishing (...) Portugal has seven regions, which in itself indicates that there is a lot to visit and get to know, but we have at least 10 reasons why it is a good choice and on the list of trips you should do in your lifetime.

We sail on secondary and shallow channels, allowing excellent views of birds at short distances without disturbing them.

During this boat trip we will be looking for dolphins outside Ria Formosa, out on the sea.




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Assessing Previously Unassessed Petroleum Provinces Using the Variable Shape Distribution (VSD) Model, Robert F. Sequence Stratigraphy as Predictive Tool in Lower Goru Fairway, Lower and Middle Indus Platform, Pakistan, Nadeem Ahmad, Paul Fink, Simon Sturrock, Tariq Mahmood, and Muhammad Ibrahim, #10404 (2012). Seismic Attributes for Prediction of Reservoir Architecture and Hydrocarbon Prospectivity: A Case Study of Zubair Formation in Bahrah Area, North Kuwait, Eman Al-Shehri, Subrata K. Quantitative Estimation of Directional Permeability Barriers as a Reservoir Heterogeneity - A New Approach Using Synthetic Core, Mahbub Alam and Larry Lines, #41518 (2015). Alammar, Ahmad Manowar, Banik Nikhil, Hanan Al-Owihan, Saifullah Tanoli, Badruzzaman Khan, Sudhakar Rao Mushnuri, and Marco Alvarez, #20118 (2011). The Use of Seismic Technologies in Different Reserve Standards: Applications of 3D Seismic and 4D Seismic to the SEC, NI-51 and PRMS Reserve Categories, Jeffrey B. Regional Structural Framework of Gabon, Derived from Public Source Gravity Data, Michael Alexander and Karim Aimadeddine, #10199 (2009). Origin of the Mid-Cretaceous Heavy Oils from the Safaniya Sandstone Reservoir, (Wasia Formation), Saudi Arabia, Ranya Algeer, Haiping Huang, and Steve R. Gradients in Sediment Geochemistry as a Constraint on Modeling Epeiric Sea Circulation, Thomas J. Up-Scaled Petrophysical Analyses Using Micro-Level Field-Of-View Petrographic Images for the Kapuni Group, Taranaki Basin, New Zealand, Aamer Alhakeem, Kelly Liu, and Waleed H. Optimization of Formation Evaluation by Integration of Advanced Surface Fluid Logging and Downhole Tools in Difficult Geological Settings, Mazwan B. Multimicrofossil Biostratigraphic Analysis of Wells A and B, Krishna - Godavari Basin, Q.


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