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  • Permeable Rock: Understanding Fluid Flow Through Sedimentary Materials
    The term that describes rock through which fluids can flow easily is permeable.

    Here's why:

    * Permeability refers to the ability of a rock or soil to allow fluids (like water, oil, or gas) to pass through its pores and fractures.

    * Porosity, on the other hand, refers to the amount of empty space within a rock.

    * While a rock can have high porosity, it might not be permeable if the pores are not interconnected.

    Examples of permeable rocks:

    * Sandstone: Has large, interconnected pores.

    * Fractured limestone: Cracks and fissures allow fluid flow.

    * Gravel: Large spaces between the particles allow easy fluid movement.

    Examples of impermeable rocks:

    * Granite: Very dense and lacks interconnected pores.

    * Shale: Fine-grained, with tiny pores that are not interconnected.

    * Clay: Has very small pores and often acts as a barrier to fluid flow.

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