Igneous Textures Flashcards
Intrusive
rocks that crystallize below the surface, slowly
Extrusive
rocks that form from cooling and crystallization above the surface, QUICKLY
Extrusive
rocks that form from cooling and crystallization above the surface, quickly
Crystalline
interlocking crystals
Phaneritic
associated with intrusive, BIG crystals b/c long time to grow due to slow cooling of magma
Aphanitic
associated with extrusive, tiny crystals due to rapid cooling near-surface = less time to grow
Glassy
No/few crystals = glassy/glossy due to lava cooling extremely rapidly
Porphyritic
Two different crystal sizes in the same rock, indicative of multi-stage cooling. Large crystals = phenocrysts
Vesicular
Cavities (vesicles) formed by trapping of gases released during crystallization of lava