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Telheiro beach Portugal

Telheiro beach Portugal

Trolltunga (die Trollzunge) in Tyssedal, Norwegen - Foto: Terje Nesthus

Trolltunga (die Trollzunge) in Tyssedal, Norwegen - Foto: Terje Nesthus

A Terceira Dimensão - Fotografia Aérea: Praia do Telheiro - Ponta do Telheiro

A Terceira Dimensão - Fotografia Aérea: Praia do Telheiro - Ponta do Telheiro

Ponta do Telheiro, do Paleozóico-Terciário, onde, entre outros pormenores, existe um grês de Silves que é branco.  A Ponta do Telheiro, com o grês branco e a descontinuidade.

Ponta do Telheiro, do Paleozóico-Terciário, onde, entre outros pormenores, existe um grês de Silves que é branco. A Ponta do Telheiro, com o grês branco e a descontinuidade.

10 best beach bars

10 best beach bars

Portugal Praia,Telheiro,Fabuloso Geologia,Algarve Portugal,Well Bedded,Obscene Geology,Planar Red,Triassic Unconformity,Yellow Sandstones

Gullfoss, iceland

O que ver na Islândia, o que visitar na Islândia

Gullfoss, iceland

[PAISAGEM]

[PAISAGEM]

moqui marbles, utah  Iron oxide concretions (Moqui marbles)        Moqui Marbles, hematite concretions, from the Navajo Sandstone of southeast Utah. Scale cube, with "W", is one centimeter square.  The Navajo Sandstone is also well known among rockhounds for its hundreds of thousands of iron oxide concretions

moqui marbles, utah Iron oxide concretions (Moqui marbles) Moqui Marbles, hematite concretions, from the Navajo Sandstone of southeast Utah. Scale cube, with "W", is one centimeter square. The Navajo Sandstone is also well known among rockhounds for its hundreds of thousands of iron oxide concretions

Praia do Telheiro The Mesozoic strata are truncated by a wave cut surface of Quaternary age, covered by various generations of eolian and coastal deposits with different degrees of consolidation. These deposits preserve different generations of coastal scarps and wave cut surfaces produced by the Quaternary sea level oscillations Good examples of syn-sedimentary and deformation structures can be observed.

Praia do Telheiro The Mesozoic strata are truncated by a wave cut surface of Quaternary age, covered by various generations of eolian and coastal deposits with different degrees of consolidation. These deposits preserve different generations of coastal scarps and wave cut surfaces produced by the Quaternary sea level oscillations Good examples of syn-sedimentary and deformation structures can be observed.

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