weathering Flashcards
what is progressive transformation?
since the earth was formed 4.5 billion years, rocks have been made up and rearranged and moved elsewhere, eventually becoming part of another rock etc.
what is the rock cycle like?
example of geological mass- transfer cycle. it involves the transfer of materials to different parts of the earth system.
what are the 5 stages of rock?
igneous rock may weather and erode to produce sediment, which lithifies to form sedimentary rock. the new sedimentary rock may become buried and form metamorphic rock. which could then partially melt to create magma. magma then solidifies to form new igneous rock.
what is the alternative pathway of igneous rock?
igneous rock could alternatively be uplifted and eroded to form new sediment and then new sedimentary rock without melting, taking a shortcut. or it could e be metamorphosed directly, without turning into sediment.
how can material enter the rock cycle?
the material can enter when basaltic rock rises from the mantle. if magma erupts and forms basalt (igneous rock), and a continental hot spot volcano.
what interactions can help the rock cycle?
wind, rain and vegetation gradually weathers the basalt
how is shale produced?
magma erupts and forms igneous rock and a continental hot spot volcano. the interaction with wind and rain and vegetation weather the basalt, breaking it into smaller pieces and altering it to create cay. as water washes over the clay, it carries it downstream, and the river reaches the sea. the clay is deposited in the mud and gets buried and packed tightly together. this results in shale.
what happens to shale?
slides below the continental shelf for millions of years, until adjacent oceanic plates subduct and the neighboring continent collides. the shale gets buried deep and as the mountain grows, the shale now moves nearer the surface, and it is metamorphosed into schist.
what happens to schist?
the crust containing the schist breaks apart and splits during continental rifting. some of the schist melts and a new felsic magma forms, which raises to the surface of the crust and freezes to create rhyolite- igneous rock.
what is weathering?
disintegration and decomposition of rocks and sediments by mechanical and chemical processes acting near or at the earth’s surface in situ.
what is erosion?
process wehreby particles of rock or soil are detached and transported by wind, ice or fire.
what is salt wedging?
growth of salt crystals. dissolves the salt in groundwater precipitates and grows as crystals in open pore spaces in the rock. pushes apart surrounding grains and so weakens the rock.
what is thermal expansion and contraction?
different minerals expand an contract at different rates. when heat of an intense forest fire bakes a rock, the outer part expands. on cooling, the layers contract. this change creates forces in the rock , breaks off in sheet-like pieces.
what is exfoliation of rocks?
spalling or surficial layers dye to the release of ithostatic pressure and expansion of rock. occurs as a result of chemical weathering.
what is mechanicl weathering?
physical disintegration of rocks into smaller fragments. salt wedgin, thermal expansion, exfolisation, root wedging, abrasion, frosting, jointing, animal attack