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Kenitiro Suguio

To the east of this assemblage, lakes can be found, partially filled with peat. Sorry, but Javascript is not enabled in your browser!

This rights cover the whole data about this document as well as its contents. The deposits are found mainly in the proximal and medial areas of the fans. They consist of rudaceous deposits, interspersed in some areas, and nearly always covered with finer-grained material. Paleolagoonar and estuary deposits in certain stretches and situations are covered by lacustrine deposits, running parallel or perpendicular to beach ridges sandy bodies from various ages. Reproduction for commercial use is forbidden.

These deposits have a flat top and are slightly inclined to the east.


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Lacustrine deposits frequently appear as surface sediments, consisting of peat, ranging in thickness from 1 to 4. The remainder was added in the regressive period that followed, giving rise to beach ridges varying in height from 14 to 16m. Learn what derived works are clicking here. 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.

Sandy beach deposits are kennitiro varying ages of the Pleistocene and Holocene and cover areas of two river basins. Some deposits, with samples of trunks, shells and peat, mainly lagoonar, estuary and lacustrine deposits, could be dated by ‘C POT.

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

The sequence of deposits makes it possible to define the recurrence of both the marine and continental processes. Rudaceous deposits are also found on the subsurface, covered over with coastal marine deposits, corresponding to the higher sea level of overyears ago.

One part of this deposit began as a barrier island sedimemtar a period of marine transgression. It is situated in the northeast of the area under investigation.

Suguio, Kenitiro 1937-

This morphology is due to deposit and erosion processes characteristic of alluvial fans. The distal deposits of the fans have a very slight representation.

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There seem to have been two major periods of aeolic activity: 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. They have a lobe morphology kenitirl a convex top, separated by low flat areas.

These sediments consist of various deposits that originated under different conditions and environments and are distributed from the foot of the scarp of the “Serra Geral” General Range to the Atlantic Ocean. 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.

This document is only for private use for research and teaching activities. 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.