describes transitions through geologic time among the three main rock types: sedimentary, metamorphic, and igneous.
Igneous Rocks
formed by magma and lava as it cools
Intrusive Igneous Rocks
formed when magma cools and solidifies before it reaches the surface
generally wholly crystalline and characterized by large crystal sizes visible to the naked eye because they cool slowly
well-formed
Extrusive Igneous Rocks
formed when magma exits (volcanic vent) and cools above (or very near) the Earth's surface
rocks that form at erupting volcanoes and oozing fissures
Types of Intrusive Igneous Rocks
diorite
gabbro
granite
pegmatite
Types of Extrusive Igneous Rocks
andesite
basalt
obsidian
pumice
rhyolite
scoria
Sedimentary Rocks
made when sediments (sand, gravel, and dirt) are pressed together over time and become a rock
formed in layers
Formation of Sedimentary Rocks
Weathering of preexisting rocks (Weathering and Erosion)
Transport of weathering products
Deposition of the material (Deposition)
Sand, dirt, clay, and/or small rocks are pressed together over time so that the space between the pieces gets smaller (Compaction)
Sediments are hardened by the precipitation of mineral matter in the pore spaces (Cementation)
Metamorphic Rocks
made from other rocks
heat and pressure help change an igneous or sedimentary rock to this kind of rock
Crystals
are different atoms that are formed in a pattern
can be big or small, fat or thin
Grains
smaller pieces of rock or sediment
grain size is something that is used a lot to help decide the rock type
Magma
molten rock
Lava
when magma already exits the volcano and starts to cool on the earth's surface
Granite
igneous rocks which were formed by slowly cooling pockets of magma that were trapped beneath the earth's surface
used for long-lasting monuments and for trim and decoration on buildings
Pumice
igneous rocks that are formed when lava is cooled quickly above ground
it is so light, many of this type of rock will actually float in water
a kind of glass and not a mixture of minerals
often used as a decorative landscape stone
Obsidian
glass-like structure
edges of this rock are very sharp
Sandstone
sedimentary rocks made from small grains of the minerals quartz and feldspar
often used as building stones
Shale
sedimentary rock formed from clay that is compacted together by pressure
used to make bricks and other material that is fired in a kiln
Limestone
sedimentary rocks that are made from the mineral calcite which came from the beds of evaporated seas and lakes and from sea animal shells
used in concrete and is an excellent building stone for humid regions
Schist
metamorphic rocks that can be formed from basalt, shale, or slate through heat and pressure
Gneiss
metamorphic rocks that may have been granite, but changed because of heat and pressure
Clastic Sedimentary Rocks
composed predominantly of broken pieces or clasts of older weathered and eroded rocks
classified based on grain size, clast, and cementing material composition (matrix), and texture
Organic Sedimentary Rocks
form from the accumulation and lithification of organic debris, such as leaves, roots, and other plant or animal material
Chemical Sedimentary Rocks
formed by chemical precipitation that begins when water traveling through rocks dissolves some of the minerals
Foliated Metamorphic Rocks
when rocks with flat or elongated minerals are put under immense pressure and the minerals line up in layers
Non-foliated Metamorphic Rocks
are formed the same way as foliated metamorphic rocks, but do not contain the minerals that tend to line up under pressure and thus, do not have a layered appearance of foliated rocks
Coal
a sedimentary rock formed over millions of years from compressed plants
"best" example of sedimentary rock
Ranks of Coal (lowest to highest)
Peat
Lignite
Bituminous
Sub-bituminous
Anthracite
Origin
a way you can classify rocks as igneous, sedimentary, or metamorphic