model that illustrates the origin of the 3 basic types of rocks & the interrelatedness of Earth’s materials and processes
igneous rock?
rock formed from the cooling and hardening (recrystallization) of molten (melted) minerals
sedimentary rock?
rock formed from weathered products of pre-existing rocks that have been transported, deposited, compacted, & cemented
metamorphic rock?
rock formed from the alteration of pre-existing rock under the influence of heat and pressure
clastic sedimentary rock?
sedimentary rocks that are made up of pieces of pre-existing rocks
chemical sedimentary rock?
breaking down of rocks by changing the molecular structure of rocks and soil.
biologic/biochemical sedimentary rock?
sedimentary rocks that form when living organisms die, pile up, and are then compressed and cemented together.
rock erosion?
the geological process in which earth materials are transported by natural forces such as wind or water.
rock deposition?
the geological process in which sediments, soil and rocks are added to a landform or landmass
rockcompaction?
layers are squeezed together and any water mixed in with the sediments is forced out
rockcementation?
the hardening and welding of clastic sediments (those formed from preexisting rock fragments) by the precipitation of mineral matter in the pore spaces.
mechanicalweathering?
also called physical weathering; it is a process that causes rocks to break down
chemicalweathering?
breaking down of rocks by changing the molecular structure of rocks and soil.
rockexfoliation?
process in which large flat or curved sheets of rock fracture and are detached from the outcrop due to pressure release
frostwedging?
happens when water gets in crack, freezes, and expands
regolith?
the layer of unconsolidated rocky material covering bedrock
soil?
the upper layer of earth in which plants grow a black or dark brown material typically consisting of a mixture of organic remains, clay, and rock particles
soil horizon?
a layer parallel to the soil surface whose physical, chemical and biological characteristics differ from the layers above and beneath.
humus?
he organic component of soil, formed by the decomposition of leaves and other plant material by soil microorganisms
bedrock?
solid rock underlying loose deposits such as soil or alluvium.
mass movement?
bulk movements of soil and rock debris down slopes in response to the pull of gravity
glacier?
a slowly moving mass or river of ice formed by the accumulation and compaction of snow on mountains or near the poles
alluvial fan?
a fan-shaped mass of alluvium deposited as the flow of a river decreases in velocity.
wind deflation?
the removal of solid particles by wind]
wind abrasion?
the process of friction caused by scuffing, scratching, wearing down, marring, and rubbing away of materials
Rock Cycle:
Model illustrating the origin of the 3 basic types of rocks and the interrelatedness of Earth’s materials and processes
Igneous Rock:
Formed from the cooling and hardening (recrystallization) of molten (melted) minerals
Sedimentary Rock:
Formed from weathered products of pre-existing rocks that have been transported, deposited, compacted, and cemented
Metamorphic Rock:
Formed from the alteration of pre-existing rock under the influence of heat and pressure
Clastic Sedimentary Rock:
Made up of pieces of pre-existing rocks
Chemical Sedimentary Rock:
Form by precipitation of minerals from water
Biologic/Biochemical Sedimentary Rock:
Form when living organisms die, pile up, and are then compressed and cemented together
Rock Erosion:
Geological process where earth materials are transported by natural forces like wind or water
Rock Deposition:
Geological process where sediments, soil, and rocks are added to a landform or landmass
Rock Compaction:
Layers are squeezed together and any water mixed in with the sediments is forced out
Rock Cementation:
Hardening and welding of clastic sediments by the precipitation of mineral matter in the pore spaces
Mechanical Weathering:
Also called physical weathering; it causes rocks to break down
Chemical Weathering:
Breaking down of rocks by changing the molecular structure of rocks and soil
Rock Exfoliation:
Process where large flat or curved sheets of rock fracture and detach from the outcrop due to pressure release