Chapter 4 Flashcards
rock composition
the proportions of different chemicals and thus the identity of minerals or glass that make up a rock
rock texture
the dimension and shape of grains and the ways that grains, and the ways the grains are arranged, oriented, and held together
igneous rocks
form through the cooling and solidification of molten rock, which is created by the melting of preexisting rock in the mantle or lower crust
magma
molten rock below the earth’s surface
lava
magma that has erupted onto the surface
sedimentary rock
form at or near the surface of the earth in two basic ways
1: when grains of preexisting rocks accumulate, are buried, and then are cemented together by minerals precipitating out of groundwater
2: when minerals precipitate out of water near the Earth’s surface, either directly or through the life function of an organism, and either form a solid mass or are cemented together laterweatheri
weathering
when preexisting rocks are broken down into their smallest pieces by processes and interactions with air, water, and living organisms
chemical and physical
Metamorphic rocks
form when preexisting rocks are subjected to physical and chemical conditions within the Earth such as the increase in pressure and temperature and or shearing at elevated temperature
forms without weathering
erosion
the grinding effects of moving ice, water, or air
rock cycle
the flux of material from one rock type to another over geologic time
involves the reuse of mineral grains or the breakdown of minerals into their constituent atoms and reuse of those atoms to make other minerals
Texture and Minerology
determine the origin of a rock
grain size
are the grains course enough to be identified