Minerals and Rocks Flashcards
memorize (30 cards)
the fundamental components of rocks
Minerals
the most abundant components of rocks on the Earth’s surface
Silicate minerals
fundamental
chemical building block of silicate minerals
Silicon tetroxide, SiO4
Minerals are classified according to their
chemical composition
are the essential building blocks of the geosphere
Minerals and rocks
is usually called silica, is one of the most common
minerals in the Earth’s crust.
Quartz
is a sodium- or calcium-rich feldspar.
Plagioclase feldspar
are rich in alkali
metal ions.
Alkali feldspar
usually occur as stubby prisms.
Alkali feldspar crystals
form
flat, book-like crystals that split into individual sheets, separating into smooth
flakes along the cleavage planes.
Micas
form prismatic or needle-like crystals.
Amphiboles
form short or columnar prismatic crystals.
Pyroxene
is a green, glassy mineral.
Olivine
is made up of calcium carbonate
Calcite
naturally occurring aggregates of minerals, rock fragments or
organic matter.
Rocks
two important
characteristics that may help to confirm the origin of a rock.
Texture and mineral composition
refers to the sizes and shapes of the component minerals or grains, and
to their collective arrangement in a rock.
Texture
refers to the crystals, mineral grains, fragments of other rocks,
and/or fossils, that make up a rock.
Composition
form when hot, molten rock (magma) cools and solidifies.
Igneous Rocks
are formed when rising magma is trapped
deep within the Earth, where it cools very slowly over many thousands or
millions of years until it finally solidifies.
Intrusive Igneous Rocks
are produced when magma is erupted at,
or very near, the Earth’s surface.
Extrusive Igneous Rocks
are formed from the eroded fragments of pre-existing
rocks, or from the skeletal fragments of once-living plants or organisms.
Sedimentary Rocks
are made up of fragments (clasts) of pre-existing
rocks.
Clastic sedimentary rocks
form when large quantities of living plants or
organisms die and accumulate.
Biological sedimentary rocks