weathering Flashcards

1
Q

what is progressive transformation?

A

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.

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2
Q

what is the rock cycle like?

A

example of geological mass- transfer cycle. it involves the transfer of materials to different parts of the earth system.

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3
Q

what are the 5 stages of rock?

A

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.

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4
Q

what is the alternative pathway of igneous rock?

A

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.

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5
Q

how can material enter the rock cycle?

A

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.

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6
Q

what interactions can help the rock cycle?

A

wind, rain and vegetation gradually weathers the basalt

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7
Q

how is shale produced?

A

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.

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8
Q

what happens to shale?

A

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.

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9
Q

what happens to schist?

A

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.

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10
Q

what is weathering?

A

disintegration and decomposition of rocks and sediments by mechanical and chemical processes acting near or at the earth’s surface in situ.

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11
Q

what is erosion?

A

process wehreby particles of rock or soil are detached and transported by wind, ice or fire.

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12
Q

what is salt wedging?

A

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.

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13
Q

what is thermal expansion and contraction?

A

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.

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14
Q

what is exfoliation of rocks?

A

spalling or surficial layers dye to the release of ithostatic pressure and expansion of rock. occurs as a result of chemical weathering.

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15
Q

what is mechanicl weathering?

A

physical disintegration of rocks into smaller fragments. salt wedgin, thermal expansion, exfolisation, root wedging, abrasion, frosting, jointing, animal attack

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16
Q

what is root wedging?

A

tree roots grow in old joints can push joints open in a process called root wedging. like breaks in sidewalks.

17
Q

what is frosting?

A

lustreless ground-glass or mat surface on rounded grains of quartz. may result in the impact of grains during wind action. freezing water bursts pipes and shatters bottles, due tow water expansion when hot. the same occurs in rocks. when water is trapped in rock, it freezes and it forces the joint open to growing.

18
Q

what is jointing?

A

rocks buried deep in the earth’s crust endure pressure due to overburden being very heavy. rocks at depth are also warmer than rocks on the surface. the squeezing of this rock decreases, and the rock becomes cooler. natural cracks form on the rock due to the removal of overburden or due to cooling. joints can break into large blocks.

19
Q

how is an animal attack mechanical weathering?

A

burrowing creatures push open cracks and move rock fragments. humans have become the most energetic agents of physical weathering. quarries, mines, roadbeds.

20
Q

what is chemical weathering?

A

alteration of change in composition of a mineral due to the action of chemical agents.

21
Q

what is included in chemical weathering?

A

dissolution, hydration reactions, relative stability of minerals during chemical weathering, hydrolysis, redox, transition metals, and organisms.

22
Q

what is dissolution?

A

the reaction between minerals and acidic or alkaline water. limestone dissolution- carbonation. some minerals dissolve rapidly only when the water is acidic. it dissolves CO2 gas in the atmosphere and it sinks down through soil containing organic debris.

23
Q

what is hydration reactions?

A

absoprtion of water. hydroysis is water breaking. causes minerals to expand.

24
Q

what is relative stability of minerals during chemical weathering?

A

not all minerals undergo chemical weathering at the same rates. in high cliamtes, it is faster. less stable.

25
Q

what is hydrolysis?

A

in the weathering of silicates, both water and carbonic acids are involved. consumes CO. weathering is the thermostat of the earth system- it controls the carbon cycle. if high CO2 increases, more weathering. if less CO2, less weathering.

26
Q

how does redox help weathering?

A

microbial action in sediment pores of water. elements lose electosn, due to the combination of oxygen. rusting of iron is an example of this.

27
Q

how do transition metals help weathering?

A

can exist in variable oxidation states. can donate or accept electrons.

28
Q

how does chemical weathering occur in organisms?

A

roots of plants, fungi, lichens, all secrete organic acids that help dissolve minerals in rocks.

29
Q

how do the 2 weatherings work together?

A

physical weathering speeds up chemical weathering. depends on the surface to volume ratio. the greater the surface area, the faster the volume of chemical weathering. if you take fresh granite and drop it, it won’t crack. take chemical weathered granite and drop it, it will crumble, therefore chemical also speeds up physical.

30
Q

what are factors that influence chemial weathering?

A

climate (temp, rainfall)
time
living organisms (acid producition, mineral decomposition)
mineral composition.

31
Q

what is soil?

A

part of regolith containing weatehred rock, water, air and humus

32
Q

why is soil important?

A

gives life. consists of rock and sediment that has been modified by weathering. interactions with organic material and rainwater- produces substrate that can support the growth of plants. soil is a type of regolith

33
Q

what is regolith?

A

debris that covers bedrock. includes both soil and accumulations of sediment that hasn’t evolved into soil yet.

34
Q

how is grain shape measured?

A

roundness and sphericity. roundness as the measure of how smooth the grain surface is depending on the transport. sphericty depends on how closely the grain shape approximates the sphere.

35
Q

what is the stage of rock maturity?

A

immature > submature > mature > supermature