LAVA MUSIC FOR DUMMIES

กดเลยยย!!!Thin basaltic lava flows normally consist of quite a few holes, or vesicles, left by bubbles of fuel frozen to the congealing liquid. Thick flows, which remain warm for prolonged intervals, could shed most in their gasoline prior to the lava congeals, and the resulting rock can be dense with several vesicles.ก่อนอ�