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Geologia Sedimentar

The deposits and processes generated in the alluvial fans began earlier than this older coastal deposits and therefore the subsurface rudaceous deposits show lower sea level than the present one. Lacustrine deposits frequently appear as surface sediments, consisting of peat, ranging in thickness from 1 to 4. There seem to have been two major periods of aeolic activity: They have a lobe morphology with a convex top, separated by low flat areas.

The distal deposits geolpgia the fans have a very slight representation.

Kenitiro Suguio (Author of Geologia Sedimentar)

They consist of rudaceous deposits, interspersed in some areas, and nearly always covered with finer-grained material. The sequence of deposits makes it possible to define the recurrence of both the marine and continental processes. They are bound on the east by another Pleistocene set of beach ridges and dunes Barrier lllcorresponding to a higher sea level ofyears ago and followed by a third formation Barrier lV with an aeolic covering and containing active dunes from the Holocene.


The rock formations appear in the form of scarps and residual elevations and underlie the Cenozoic sediments that cover the greater part of the area under investigation. To the east of this assemblage, lakes can be found, partially filled with peat.

Some deposits, with samples of trunks, shells and peat, mainly lagoonar, estuary and lacustrine deposits, could be dated by ‘C POT.

It is situated in the northeast of the area under investigation.

These sediments consist of various deposits that originated under different conditions seeimentar environments and are distributed from the foot of the scarp of the “Serra Geral” General Range to the Atlantic Ocean. Sandy beach deposits are from varying ages of the Pleistocene and Holocene sedimemtar cover areas of two river basins. Reproduction for commercial use is forbidden. One part of this deposit began as a barrier island during a period of marine transgression.

Depósitos cenozoicos costeiros e a morfologia do extremo sul de Santa Catarina

These deposits have a flat top and are slightly inclined to the east. Sorry, but Javascript is not enabled in your browser! Learn what derived works are clicking here.


The beologia are found mainly in the proximal and medial areas of the fans. Any uses or copies of this document in whole or in part must include the author’s name.

Kenitiro Suguio

Rudaceous deposits are also found on the subsurface, covered over with coastal marine deposits, corresponding to the higher sea level of overyears ago.

Belonging to the Pleistocene is a large formation of aeolic origin that reaches an altitude of m and is supported by rocks of the Palermo Formation. This rights cover the whole data about this document as well as its contents.

Paleolagoonar and estuary deposits in certain stretches and kentiiro are covered by lacustrine deposits, running parallel or perpendicular to beach ridges sandy bodies from various ages. The remainder was added in the regressive period that followed, giving rise to beach ridges varying in height from 14 to 16m. This morphology is due to deposit and erosion processes characteristic of alluvial fans.

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