esq2 Flashcards

1
Q

three main sources of heat of the earth

A

primordial heat, decay of radioactive isotopes, tidal friction

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2
Q

leftover heat from the formation of Earth

A

primordial heat

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3
Q

comprises the lithosphere

A

crust and uppermost part of the mantle

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4
Q

below the lithosphere, 180 km and contains thick hot molten rocks or magma

A

asthenosphere

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5
Q

outermost layer of the earth where life exists

A

crust

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6
Q

the crust that makes up the continents, and is 40-70km thick

A

continental crust

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7
Q

below the crust, a semisolid, rocky and very hot layer, 2900km thick, makes up 80% of earth and carries most of its mass.

A

mantle

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8
Q

composition of the mantle

A

ferro-magnesium silicate rocks

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9
Q

two distinct layers of the core

A

outer and inner core

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10
Q

the only layer in the Earth that is liquid, which is made up of molten nickel and iron. about 2270km thick with temperatures ranging from 3700C-4300C.

A

Outer core

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11
Q

1220km as its diameter, composed of mostly solid iron, extremely hot and about 6000C

A

Inner core

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12
Q

Boundaries between the layers of the Earth

A

Conrad discontinuity (upper-lower crust)
Mohorovicic discontinuity (crust-upper mantle)
Repetti discontinuity (Upper mantle-lower mantle)
Gutenberg discontinuity (lower mantle-outer core)
Lehmann discontinuity (outer core-inner core)

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13
Q

places where magma can be formed

A

mid-oceanic ridges
mantle plumes
subduction zones

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14
Q

hot molten rock containing chemical elements from uppermost mantle called asthenosphere

A

magma

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15
Q

an extent of a fluid’s resistance to flow

A

viscosity

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16
Q

explained why certain minerals occur together while others are almost never linked with one another

A

Norman L. Bowen

17
Q

based on this, one can conclude from the minerals in a rock the conditions under which rock had formed

A

Bowen’s reaction series

18
Q

discontinuous branch

A

ferromagnesian minerals: olivine, pyroxene, amphibole, biotite mica, potassium-rich feldspar, muscovite mica, quartz

19
Q

continuous series or branch

A

non ferromagnesian minerals: calcium-rich plagioclase feldspar, and sodium-rich plagioclase feldspar

20
Q

ultramafic

A

the composition of the mantle (peridotite) and rarely found on the surface. Contains mostly olivine, pyroxene, and a small amount of calcium-rich plagioclase feldspar.

21
Q

mafic

A

Contains mostly dark, ferromagnesian minerals such as: olivine, pyroxene, as well as, calcium-rich plagioclase feldspar, and small amounts of amphibole minerals. These
rocks tend to be dark and denser, such as the rock, Basalt.

22
Q

process of generating one or more subordinate magmas from single parent magma

A

magmatic differentiation

23
Q

chemical process in which the structure of the liquid, such as magma, changes due to crystallization

A

crystal fractionation

24
Q

processes of crstal fractionation

A

crystal settling, partial melting

25
Q

when heavier minerals crystallize first and settles down while the less dense minerals crystallize at the final stages

A

crystal settling

26
Q

happens when two different magmas rises up with the more buoyant mass overtakes the slower rising body

A

magma mixing

27
Q

mixes the two different parent magmas, producing a single and intermediate magma

A

convective flow

28
Q

a reaction that occurs when the crust is mixed up with the rising magma. When the magma rises up to the surface, the surrounding rocks may dissolve, and eventually mixes with magma. This produces a change in the chemical composition of the magma

A

assimilation or contamination of magma by crustal rocks.

29
Q

mineral composition of metamorphic rocks are influenced by:

A

mineral composition of the parent rock
composition of the liquid that was present
amount of pressure and temperature during metamorphism

30
Q

pressure applied to rock is not equal in all directions

A

differential stress

31
Q

pervasive and planar structure that results from nearly parallel alignment of sheet silicate minerals layering the rock

A

foliation

32
Q

formed when heat is the main agent of metamorphism, composed of mosaic roughly equidimensional and equigranular minerals

A

non-foliated metamorphic rock