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20 Cards in this Set

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  • Back
sediments
loose materials, such as rock fragments, mineral grains, and the remains of once-living plants and animals, that have been moved by wind, water, ice, or gravity
nonfoliated
describes metamorphic rock, such as quartzite or marble, whose mineral grains do not line up in parallel layers
foliated
describes metamorphic rock, such as slated and gneiss, whose mineral grains line up in parallel layers
granitic
describes generally light-colored, silica-rich, poor in magnesium and iron, less dense than basaltic
basaltic
describes dense, dark-colored igneous rock form from magma, rich in magnesium and iron, poor in silica
rock
mixture of one or more minerals, rock fragments, volcanic glass, organic matter, or other natural materials; can be igneous, metamorphic, or sedimentary
organic
made from the remains of once-living things
chemical
dissolved minerals that come out of a solution; not made from preexisting rocks
conglomerate
rock that is rounded (sedimentary)
breccia
rocks with sharp edges (sedimentary)
detrital
form from broken fragments of other rocks; sediments are compacted and cemented together to form solid rock
erosion
movement of weathered materials
igneous
forms when hot magma/lava cools and hardens
extrusive
describes fine-grained igneous rock that forms when magma cools quickly at or near Earth's surface
intrusive
describes a type of igneous rock that generally contains large crystals and forms when magma cools slowly beneath Earth's surface
cementation
sedimentary rock-forming process in which sediment grains are held together by natural elements that are produced when water moves throughout rock and soil
compaction
process that forms sedimentary rocks when layers of sediments are compressed by the weight of the layers above them
sedimentary
forms when sediments are compacted or cemented together or when minerals form from solutions
metamorphic
forms when heat, pressure, or fluids act on igneous, sedimentary, or other metamorphic rock to change its form, composition, or both
rock cycle
model that describes how rocks slowly change from one form to another through time