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  2. Phaneritic texture forms from the slow cooling (allows crystals to grow large) of magma deep in the Earth’s crust, while aphanitic texture forms on or near the Earth’s surface where fast cooling doesn’t allow crystals to grow large. Therefore, you can tell the cooling history by considering these two textures.
    geologybase.com/phaneritic-vs-aphanitic/
    Aphanitic rocks have fine-grained textures, making individual mineral crystals hard to see without magnification. Phaneritic rocks have coarse-grained textures, making the individual mineral crystals visible. Aphanitic rocks form from the rapid cooling of magma, while phaneritic rocks form from slow cooling.
    askanydifference.com/difference-between-aphaniti…
    In summary, the main difference between aphanitic and phaneritic textures lies in the size of the mineral crystals and the cooling rate of the igneous rocks. Aphanitic rocks have fine-grained textures with small crystals due to rapid cooling, while phaneritic rocks have coarse-grained textures with larger crystals due to slow cooling.
    www.numerade.com/questions/explain-the-differen…
    Phaneritic rocks are entirely crystalline (holocrystalline), having mineral grains that can be observed without the aid of a hand lens or microscope, whereas aphantic rocks have mineral grains that cannot be observed with the unaided eye.
    www.britannica.com/science/aphanitic-texture
     
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