Linked from

The 7 pages that link to Phaneritic texture, each with the reason it gives.

• GraniteRelated: Granite’s coarse grains record crystallization slow enough for crystals to grow.

• Igneous rockRelated: Visible crystals commonly indicate slow cooling beneath the surface.

• GabbroRelated: Slow underground cooling gives gabbro its coarse, visible crystals.

• Intrusive rockRelated: Slow underground cooling commonly gives intrusive rocks this coarse-grained texture.

• DioriteRelated: Slow underground cooling gives diorite its visible, coarse mineral grains.

• TonaliteRelated: Slow cooling underground produces tonalite’s coarse-grained texture.