Oceanite (from Mauna Loa) – a basalt with >40% mafic phenocrysts, and all the phenocrysts are olivine
Ankaramite (from Hualālai) – a basalt with >40% mafic phenocrysts, and those phenocrysts consist of olivine and pyroxene olivine
Pyroxene crystals, weathered out of ankaramite lavas, East Maui SW rift zone
Outer, weathered surface of ankaramite from Rarotonga, Cook Islands pyroxene
Freshly broken surface of ankaramite from Rarotonga, Cook Islands olivine amygdule (former vesicle, now filled with some sort of secondary mineral) pyroxene
Vesicular basalt (from Kohala) with lots of little clusters of plagioclase feldspar phenocrysts (and a few olivine phenocrysts). plagioclase feldspar vesicle (frozen bubble) olivine
Very fine-grained (almost glassy) basalt, from Wai‘anae
Fragment of pāhoehoe lava showing the rapidly-chilled (and therefore glassy) outer surface, and the more slowly-cooled (and therefore crystalline) interior