4: Sedimentary Structures

Sedimentary Geology: Rocks, Environments and Stratigraphy · LibreTexts

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    From LibreTexts, under CC BY-SA 4.0, as the source states it; its equations are written in TeX, which the PDF shows typeset. This page at LibreTexts.

    4: Sedimentary Structures

    Sedimentary structures are important because they tell us about processes that were operating during the deposition of that sediment. Things like flow velocity, depth, and direction can be determined from some sorts of structures. From there, we can start to make some educated guesses about what sorts of depositional environments these processes were taking place in. But, the first step is having the vocabulary to describe what you are seeing.

    Learning Objectives
    • Identify common sedimentary structures
    • Interpret appropriate sedimentary structures to determine paleoflow direction
    • Interpret and describe the processes responsible for and recorded by sedimentary structures
    • Use appropriate sedimentary structures to determine way up and top/bottom of beds

    Chapter thumbnail shows eolian sand dunes in Death Valley National Park (Michael C. Rygel via Wikimedia Commons; CC BY-SA 4.0).


    This page titled 4: Sedimentary Structures was last modified on Sun, 04 Jan 2026 17:20:00 GMT and is shared under a CC BY-SA 4.0 license and was authored, remixed, and/or curated by Michael Rygel and Page Quinton.