Stylolites in Mississippian limestone

Stylolites (pressure solution seams) in limestone of Mississippian age, exposed on the side of a rounded boulder in Hyalite Canyon, Gallatin Range, Montana. These stylolites, like most, are bedding-parallel, and thus most likely formed due to the weight of the overlying rock. Calcite, the dominant mineral, goes into solution under pressure, and insoluble material, like organic matter and clay, accumulates along the dissolution surface, producing a dark, wiggly line. Here, multiple stylolites have converged and overprinted one another, resulting in a mutli-level “oscilloscope” look.

0 thoughts on “Stylolites in Mississippian limestone”

  1. Thank you for your image and explanations. I am a geologist in Turkey. I study evaporites in Tuz Gölü basen. do you have another picture about stylolites

    Reply
    • Oh. I’m sure I’ve got a few others kicking around here somewhere. I’ll have a look-see, and post them in the future if I find any worth sharing.

      Reply

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