ʻO ka pōhaku maoli e pili ana i nā pōhaku sedimentary a metamorphic carbonate e like me ke kinikini, dolomite, limestone, pōhaku one, shale and slate. ʻO ka pōhaku maoli o kēia wā e ʻeli ʻia mai ka pōhaku maoli, a laila ma hope o ke ʻano o ka hana ʻana, E pili ana i ka mea i hoʻohana ʻia i ka hoʻonaninani hale, ʻo ka hale maʻamau o nā pōhaku kūlohelohe ka nui o ka granite a me ke kinikini ʻelua ʻano.
ʻO ka Granite he pōhaku igneous, i kapa ʻia hoʻi ka pōhaku plutonic acid crystalline. ʻO ia ka pōhaku igneous i hoʻolaha nui ʻia, e ka feldspar, quartz a me ka mica haku, pōhaku paʻa paʻa. ʻO ka Granite ka nui o ka silicon dioxide, ma kahi o 65%-75% o ka pōhaku i kapa ʻia ʻo ia ka pelemaka lalo a i ʻole ka lua pele o ka crystallization pele o ka pōhaku.
Marble is a metamorphic rock formed by high temperature and pressure in the crust of the Central Plain. The internal force of the Earth’s crust causes the qualitative changes of the original rocks, i. e. the structure, structure and mineral composition of the original rocks are changed. New Rocks formed by metamorphism are called metamorphic rocks.