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  • Sandstone Streak and Hardness: A Guide to Mineral Composition
    The streak of sandstone and hardness depend on the minerals present in the sandstone. Here's why:

    * Streak: Sandstone is a clastic sedimentary rock, meaning it's formed from fragments of other rocks. The color of the streak, which is the color of the powder left behind when rubbed on a streak plate, is determined by the dominant mineral in the sandstone.

    * Quartz Sandstone: Will have a white or colorless streak because quartz is colorless and has a hardness of 7.

    * Feldspar Sandstone: Will have a white or slightly pink streak because feldspar is usually white or pink and has a hardness of 6.

    * Arkose Sandstone: Will have a reddish or pink streak if it contains a significant amount of feldspar.

    * Greywacke Sandstone: Will have a dark gray streak because it contains a mixture of quartz, feldspar, and rock fragments.

    * Hardness: The hardness of sandstone varies greatly depending on the minerals present and their cementing material.

    * Quartz Sandstone: Is harder because quartz is a hard mineral.

    * Feldspar Sandstone: Is softer because feldspar is less hard than quartz.

    * Arkose Sandstone: Is also softer than quartz sandstone.

    * Greywacke Sandstone: Is generally softer because it contains a greater variety of softer minerals.

    However, it's important to note that:

    * Sandstone is often porous and friable, meaning it's relatively soft and easily broken.

    * The hardness can also be influenced by the cementing material that binds the sand grains together. This can be calcite, silica, iron oxides, or other minerals.

    In summary: You can't determine the streak and hardness of sandstone just by knowing it's "sandstone." You need to consider the specific minerals present and the type of cementing material.

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