Resumo (PT):
Abstract (EN):
Geomorphological evidence for the Pleistocene glaciation of Serra Amarela (Peneda-Gerês National
Park) was provided by Coudé-Gaussen in 1981. However, the limits of the glaciated area are imprecise for
glacial reconstruction. This mountain is characterized by its W-E asymmetric topography and by the dominance
of granitic lithology over restricted metamorphic outcrops. The steep western slopes are dominated by fluvial
and relict periglacial landforms, but the steep eastern slopes show evidence of former glacial erosion and
deposits, particularly in the Ramisquedo glacial cirque. Fluvioglacial and slope deposits are frequently observed
on the valley floors and mountainsides. This work presents a new geomorphological map of the Serra Amarela,
accomplished through the analysis and interpretation of high-resolution LiDAR data, complemented by
laboratory analysis and fieldwork validations of the deposits. This new map and data will allow the definition of
the Glacial Maximum Extent (GME), ice thickness and Equilibrium-Line Altitude for the Serra Amarela glaciation.
Language:
Portuguese
Type (Professor's evaluation):
Scientific