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Authors
Advisor(s)
Abstract(s)
Located in central Algarve, the Rocha da Pena (RP) Classified Site constitutes a place of
renowned scientific importance for several disciplines. The study area involves terrains
belonging to the Hesperian Massif and to the Algarve Basin. The ages of the units found in
the study area range from the topmost Lower Carboniferous to the Quaternary, presenting
two major stratigraphic hiatuses – the first between the lowermost Upper Carboniferous
and Upper Triassic and the second between the Lower Jurassic and, at least, the Pliocene.
Several factors, such as the lithology, stratigraphy, tectonics, geomorphology, hydrology
and climate, acted together to produce the RP, which consists of a residual and structural
upland. Fracturing along an E-W direction controlled the alignment of both the
topography and the drainage network in the area. Structurally, the RP consists of an
anticline, which axis bears an E-W trend inherited from the Upper Cretaceous N-S
compressive phase. Vertical fluvial erosion resulting from the uplift of the Algarve Ridge
and differential erosion associated to the uneven resistance of the lithologic units and its
stratigraphic order isolated the RP from the neighbouring terrains during Upper Pliocene
times. The RP constitutes an example of karst topography that has been preserved
throughout the geologic time due to karst immunity phenomena and to a paleoclimatic
setting unfavourable to its erosion.
Given its geologic peculiarities and grandeur, which kindles the curiosity of numerous
visitors, the RP should be considered a valuable piece of geologic heritage and, as such, it
is a legacy that should be promoted and preserved for the future generations. On this
account, several partnerships were forged with a number of institutions in order to
develop scientific and educational material and activities rooted on the fields of
geodiversity and geoconservation.
Description
Dissertação mest., Biologia e Geologia, Universidade do Algarve, 2006
Keywords
Teses Geologia Relevo Carsificação Divulgação científica Geoconservação Portugal Bacia algarvia