Chapter 7: The Rock Cycle Flashcards

1
Q

Define ‘Bedding’.

A

The layered arrangement of strata in a body of sediment or sedimentary rock.

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2
Q

Define ‘Biogenic sediment’.

A

Chemical sediment formed as a result of biochemical reactions in water.

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3
Q

Define ‘Burial metamorphism’.

A

Metamorphism caused solely by the burial of sedimentary or pyroclastic rocks.

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4
Q

Define ‘Cementation’.

A

The joining together of particles in a loose sediment through the addition of a cementing agent.

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5
Q

Define ‘Chemical sediment’.

A

Sediment formed by precipitation (by processes such as evaporation) of minerals from solutions in water.

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6
Q

Define ‘Chemical weathering’.

A

The decomposition of rocks through chemical reactions such as hydration and oxidation.
The principal agent is a weak solution of carbonic acid (H2CO3) that is formed when rainwater and groundwater dissolve carbon dioxide.

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7
Q

Define ‘Clastic sediment’.

A

The loose fragmented debris produced by the mechanical breakdown of older rocks. The four main size classes are gravel, sand, silt, and clay.

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8
Q

Define ‘Clay’.

A

The smallest clastic particles in sediment. The term is also used for a family of minerals.

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9
Q

Define ‘Compaction’.

A

Reduction of the volume of sediment as a result of increased pressure.

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10
Q

Define ‘Contact metamorphism’.

A

Temperature- driven metamorphism adjacent to an intrusive igneous body.

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11
Q

Define ‘Correlation (stratigraphic)’.

A

Determination of the equivalence of age of the succession of strata found in two or more different areas.

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12
Q

Define ‘Crystallization (of magma)’.

A

The set of processes whereby crystals of individual mineral components nucleate and grow in a cooling magma.

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13
Q

Define ‘Denudation’.

A

The sum of the weathering, mass-wasting, and erosional processes that result in the progressive lowering of the Earth’s surface.

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14
Q

Define ‘Deposition (of sediment)’.

A

Accumulation of sediment following transport.

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15
Q

Define ‘Diagenesis’.

A

The various low-temperature and low-pressure changes that happen to a sediment after deposition.

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16
Q

Define ‘Erosion’.

A

The complex group of related processes by which rock is broken down physically and chemically and the products are moved.

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17
Q

Define ‘Facies (metamorphic)’.

A

The assemblage of minerals formed during metamorphism of a rock of a given composition subjected to a given temperature and pressure.

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18
Q

Define ‘Foliation’.

A

The planar texture of mineral grains, principally micas, produced by metamorphism.

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19
Q

Define ‘Geologic time scale’.

A

Numerical time scale fitted to the relative ages of the geologic column.
The geologic column summarizes in chronological order the succession of known rock units determined through the principles of stratigraphy, stratigraphic correlation, and cross-cutting relationships.

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20
Q

Define ‘Gravel’.

A

The coarsest particles of clastic sediment.

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21
Q

Define ‘Igneous rock’.

A

Rock formed by the cooling and consolidation of magma.

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22
Q

Define ‘Joint’.

A

Sheet-like fractures in rock.

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23
Q

Define ‘Landslide’.

A

Any perceptible downslope movement of a mass of bedrock or regolith, or a mixture of the two.

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24
Q

Define ‘Lithification’.

A

The processes by which sediment and soil become rock.
The first stage is burial and compaction. Loose grains of sediment adhere to one another as a result of cementation or recrystallization.

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25
Q

Define ‘Lithology’.

A

Description of a rock on the basis of color, mineralogical composition, and grain size.

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26
Q

Define ‘Mass wasting’.

A

The movement of regolith downslope by gravity without the aid of a transporting medium.
The composition and texture of the sediment involved, the amount of water and air involved, and the steepness of the slope influence the type and velocity of movement.

27
Q

Define ‘Metamorphic rock’.

A

Rock whose original compounds or textures, or both, have been transformed to new compounds and new textures by reactions in the solid state as a result of high temperature, high pressure, or both.
Metamorphism describes changes in mineral assemblage and texture that occur in the solid state, at temperatures above 150°C and pressures in excess of 300 MPa. The upper limit to metamorphism is reached when rock melting begins.

28
Q

Define ‘Metamorphism’.

A

All changes in mineral assemblage and rock texture, or both, that take place in sedimentary and igneous rocks in the solid state within the Earth’s crust as a result of changes in temperature and pressure.

29
Q

Define ‘Metasomatism’.

A

The metamorphic pro- cess in which abundant fluids change the composition and texture of a rock.

30
Q

Define ‘Physical (mechanical) weathering’. Give examples.

A
The disintegration (physical breakup) of rocks.
Involves processes such as jointing, frost wedging, precipitation of salts in fractures, fire breakage, and wedging by plant roots.
31
Q

Define ‘Recrystallization’.

A

The formation, in the solid state, of new crystalline minerals grains in a rock.

32
Q

Define ‘Regional metamorphism’.

A

Metamorphism affecting large volumes of crust and involving both mechanical and chemical changes.

33
Q

Define ‘Regolith’.

A

The irregular blanket of loose, noncemented rock particles that covers the Earth.

34
Q

Define ‘Rock cycle’.

A

The cyclic movement of rock material, in the course of which rock is created, destroyed, and altered through the operation of internal and external Earth processes.

35
Q

Define ‘Sand’.

A

Clastic particles intermediate in size between gravel and silt.

36
Q

Define ‘Sediment’.

A

Regolith that has been transported by any of the external processes.

37
Q

Define ‘Sedimentary rock’.

A

Any rock formed by chemical precipitation or by sedimentation and cementation of mineral grains transported to a site of deposition by water, wind, ice, or gravity.
Bedding and the presence of fossils are typical features of sedimentary rock. Sedimentary rock contains information about the environments in which the sediment was formed, transported, deposited, and lithified.

38
Q

Define ‘Silt’.

A

Fine clastic particle intermediate in size between sand and clay.

39
Q

Define ‘Stratigraphy’.

A

The study of strata.

Stratigraphy is based on the principles of original horizontality, superposition, and lateral continuity.

40
Q

Define ‘Stratum (pl. strata)’.

A

A distinct layer of sediment that accumulated at the Earth’s surface.
Each stratum or bed differs from adjacent beds because of changes that occurred in the environment as the sediment accumulated.

41
Q

Define ‘Stress’.

A

Force per unit area acting on a body.

42
Q

Define ‘Unconformity’.

A

A substantial break or gap in a stratigraphic sequence that marks the absence of part of the rock record.
The three important kinds of unconformities are nonconformities (sediment deposited on igneous or metamorphic), angular unconformities (uplifting and erosion), and disconformities (erosion).

43
Q

Define ‘Weathering’.

A

The chemical alteration and mechanical breakdown of rock materials during exposure to air, moisture, and organic matter.

44
Q

The locations where clastic sediment is deposited are largely controlled by plate tectonics. They include …?. The deposition of chemical and biogenic sediment is not as strongly influenced by plate tectonics because it occurs in open aquatic environments.

A

Low- lying rift valleys, structural basins in mountain ranges, and deep oceanic trenches in subduction zones near continents.

45
Q

The four classes of clastic sedimentary rock are …?, which form from gravel, sand, silt, and clay, respectively.

A

Conglomerate, sandstone, siltstone (or mudstone), and shale.

46
Q

Chemical sedimentary rock results from the lithification of chemical sediment. ___, which forms from lithified shells and other skeletal material from marine organisms, is the most important rock that forms from the lithification of biogenic sediment.

A

Limestone.

47
Q

Chemical weathering can turn K-feldspar to …?

A

Clay. This can happen especially in granite, which is high in k-feldspar.

48
Q

Stratigraphic correlation is …?

A

The determination of equivalence in age of the succession of strata found in two or more different areas.

49
Q

Using ___ ___to establish the numerical ages of certain rock units, scientists have been able to fit a scale of numerical time to the geologic column.

A

Radiometric dating.

50
Q

Igneous rock textures form under uniform stress because igneous rocks crystallize from liquids, which cannot sustain differential stress. Is the same true for metamorphic rocks?

A

In contrast, the textures of many metamorphic rocks record evidence of differential stress, most commonly as foliation, a layered texture that results from the alignment of platy or elongate minerals.

51
Q

What determines the assemblage of minerals that will develop in metamorphic rocks?

A

The starting composition of a rock, in combination with the temperature and pressure of metamorphism.

52
Q

The three most important kinds of metamorphism are ___, ___, and ___ metamorphism. They differ in conditions of temperature, pressure, and differential stress, and in the relative importance of mechanical deformation and chemical recrystallization.

A

Contact, burial, and regional.

53
Q

What is Mechanical deformation? Chemical recrystallization?

A

Mechanical deformation includes grinding, crushing, and the development of foliation.
Chemical recrystallization includes changes in mineral composition, the growth of new minerals, and losses of H2O and CO2 that occur with metamorphism.

54
Q

Metamorphic rocks are named on the basis of texture and mineral assemblage. The products of the metamorphism of ___ are slate, phyllite, schist, and gneiss, in order of increasing metamorphic grade.

A

Shale.

55
Q

___ undergoes metamorphism under conditions where H2O can enter the rock and form hydrous minerals, resulting in the metamorphic rocks greenschist, amphibolite, and granulite.

A

Basalt.

56
Q

The metamorphic derivatives of ___ and ___ are marble and quartzite, respectively; they are typically monomineralic and nonfoliated.

A

Limestone and sandstone.

57
Q

The metamorphic facies concept holds that …?

A

For a given range of temperature and pressure, and a given rock composition, the assemblage of minerals formed during metamorphism is always the same.
(More in Chapter Summary, point 16?)

58
Q

Melting leads to the development of three main magma types, ___, ___, and ___, the properties of which are mainly determined by their compositions. Partial and fractional melting can lead to variations in magma types.

A

Basaltic, andesitic, and rhyolitic.

59
Q

Cooling and crystallization, in which crystals nucleate and grow in a cooling magma, combine with composition to determine the properties of igneous rock. What does the rate of cooling influence?

A

The rate of cooling influences how large the individual mineral grains eventually grow.

60
Q

When magma or lava of a given composition solidifies, the mineral assemblage that forms is the same for intrusive and extrusive rock; the differences are textural. How are volcanic and plutonic textures characterized?

A

Volcanic rock is characterized by fine grain size or glassy texture, whereas plutonic rock tends to be coarse-grained because the magma cools slowly.

61
Q

What rocks do basaltic, andesitic, and rhyolitic magma yield?

A

Basaltic magma yields the mafic volcanic rock basalt and its plutonic equivalent, gabbro. Andesitic magma yields the intermediate volcanic rock andesite and its plutonic equivalent, diorite. Rhyolitic magma yields the felsic volcanic rock rhyolite and its plutonic equivalent, granite.

62
Q

What contributes to the diversity of igneous rock types?

A

Differences in texture that develop during cooling and crystallization, and partly from partial or fractional melting, which can lead to the separation of melt from residual solid rock of a different composition. Fractional crystallization also contributes to the diversification of igneous rock types.

63
Q

What five main factors interact to determine the character of landforms?

A

Process, climate, lithology, relief, and time.
The constant changes reflect ongoing interactions between the internal forces of plate tectonics, isostasy, and volcanism that uplift the lithosphere, and the external forces of denudation that wear it down. Denudation begins as soon as a mountain range is uplifted, and continues long after active tectonic uplift has ceased.

64
Q

How is basaltic, andesitic and rhyolitic magma formed?

A

Basaltic: Partial melting of mantle that erupts where curst is splitting, i.e. mid-ocean spreading centres and above mantle hotspots.
Andesitic: Wet partial melting of mantle overlying subducting oceanic plate.
Rhyolitic: Melting at base of continental crust. Assimilates silica-rich crustal material as rising.