Physical Geology Flashcards

unit 1

1
Q

Geology

A

the study of the Earth
* physical geology is concerned with them materials and processes which compose and operate on the surface of, and within, Earth

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2
Q

Principal subsystems of the earth

A

atmosphere
biosphere
hydrosphere
geosphere

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3
Q

Plate tectonic theory

A

lithosphere is composed of rigid plates that diverge, converge, or slide sideways past one another as they move over the asthenosphere

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4
Q

Uniformitarianism

A

forms a cornerstone of geology
* principle states that the laws of nature have remained unchanged through time and thus, that the processes observed today have also operated in the past, though possibly at different rates

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5
Q

Plate movement is ____

A

the driving mechanism of the rock cycle

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6
Q

Rock

A

a solid aggregate of one or more minerals, as well as non-crystalline matter such as natural glass or organic material like coal

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7
Q

Igneous rocks

A

form from the crystallization of magma as it cools, from material that is thrown out of a volcano

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8
Q

Intrusive igneous rock

A

crystallizes beneath the earth’s surface

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9
Q

Extrusive igneous rock

A

crystallizes and cools at the earth’s surface.
* can form as glass or ash

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10
Q

Sedimentary rocks

A

typically deposited in layers formed from:
* rock/mineral fragments
* precipitation of minerals from solution
* the compaction of plant and animal remains

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11
Q

Metamorphic rocks

A

form from alteration of other rocks, usually by:
* heat
* pressure
* chemically active fluids

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12
Q

The core

A

composed of iron and a small amount of nickel

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13
Q

The asthenosphere

A

behaves plastically and flows slowly
* composed primarily of peridotite, an igneous rock made of olivine
* surrounds lower mantle
* partial melting generates magma

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14
Q

The crust

A
  • thick continental crust
  • thin, denser oceanic crust
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15
Q

The lithosphere

A
  • crust and upper mantle make up the lithosphere
  • forms the solid outer layers of the earth
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16
Q

Plate tectonics is ____

A

the unifying theory of geology
* heat-transfer within the asthenosphere, moves the plates
* plates separate, mostly at oceanic ridges
* collide and are subducted into interior at oceanic trenches

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17
Q

Alfred Wegener

A

proposed continental drift hypothesis
* however, failed to provide a convincing mechanism
* continents have moved in the past
* noticed that Africa and South America fit
* he postulated that all landmasses were
originally united into a supercontinent
named Pangaea

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18
Q

Support of plate tectonics

A
  • volcanism
  • seismicity
  • mountain building
  • climatic changes
  • animal and plant distributions
  • distributions of natural resources
19
Q

Continental crust

A
  • less dense
  • much thicker than oceanic crust
  • helps explain why mountains on land stand higher on continents than in ocean basins
20
Q

Continental crust floats

A

isostacy: crust floats in the denser mantle
* all crust is less dense than the mantle
* oceanic crust is denser and floats lower
* mountains are high because they are less dense

21
Q

Isostatic rebound

A
  • glaciers melt or mountains erode away
  • crust rises back up to equilibrium level
  • rebound occurs slowly
22
Q

Divergent

A

form when plates move away from one another
* new oceanic lithosphere is forms at the
opening rift
* most occur along the crests of oceanic ridges
* also present under continents during the early stages of continental breakup

23
Q

Convergent

A

places where two plates collide
* oceanic-oceanic: is where two oceanic plates collide, one ocean plate will subduct beneath the margin of the other plate
* oceanic-continental: oceanic plate and a continental plate collide, the oceanic plate will subduct
* continental-continental: when two continents collide, neither plate will subduct

24
Q

Oceanic-oceanic convergent boundary

A
  • one oceanic plate is subducted beneath the other
  • a volcanic island arc forms on the non-subducted plate
  • oceanic trench forms where the subduction is taking place
  • the volcanoes result from rising magma produced by the partial melting of the subducting plate
25
Q

Oceanic-continental convergent boundary

A
  • oceanic plate and continental plate converge
  • denser oceanic plate is subducted under the continental plate
  • chain of volcanoes forms on non-subducted plate
  • oceanic trench forms
26
Q

Continental-continental convergent boundary

A
  • when ocean floor separating continents is all subducted, continents converge
  • results in a collision between the two continents
  • neither plate will subduct
  • continents are welded together to form an interior mountain chain
27
Q

Transform

A
  • plates slide laterally (sideways) past each other along faults
  • these boundaries change one type of motion between plates into another type of motion
28
Q

Hot spots

A
  • a stationary column of magma, from deep within the earth
  • has slowly risen to the surface and formed a volcano
  • enable geologists to determine plate motion
  • Yellowstone
29
Q

Mantle plumes

A
  • remain stationary
  • while plates move over them, trail of extinct and progressively older volcanoes that record the movement of the plate is left
30
Q

Mineral deposits

A
  • many of the world’s major metallic ore deposits are associated with convergent and divergent plate boundaries
  • hydrothermal activity, often volcanic
31
Q

Continental accretion

A
  • process of adding material to a continent
  • common along convergent oceanic-continental plate boundaries
32
Q

Mineral

A
  • natural
  • inorganic
  • crystalline solid
  • characteristic physical properties
  • specific chemical composition
33
Q

Most common minerals are made up of ___, ___, and one or more other elements.

A

oxygen, silicon

34
Q

Silicate minerals

A

composed of the silica tetrahedra
most minerals are silicates (compounds of
silicon and oxygen, and other elements)

35
Q

Ferromagnesian silicates

A

made up of iron and or magnesium, combined with other elements
dark in color and dense
olivine and biotite

36
Q

Non-ferromagnesian silicates

A

lack iron and magnesium
light colored

37
Q

Carbonate minerals

A

all carbonate minerals have the carbonate radical (CO³)-² as in calcite (CaCO³) and dolomite [CaMg(CO³)²]
found mostly in the sedimentary rocks limestone and dolostone
carbonates are derived from the shells and hard parts of marine organisms or are precipitated from seawater as evaporites

38
Q

Native elements

A

composed of a single element
gold, copper and diamonds

39
Q

Sulfide minerals

A

contain sulfur plus a metallic element as in
galena (PbS) and pyrite (FeS²)
commonly form along mid-oceanic ridges

40
Q

Sulfates

A

have the sulfate radical (SO4 -²) as in gypsum (CaSO4 2H2O)
common in deserts, forming from evaporation of water

41
Q

Mineral cleavage

A

refers to the breakage or splitting of mineral crystals along one or more smooth planes determined by atomic structure

42
Q

Number of cleavages and direction
1
2 at right angles
3 at right angles
3 at not right angles
4
6

A

Cleavage name
micas (biotite)
prismatic - feldspars
cubic - halite and galena
rhombohedral - calcite and dolomite
octhahedral - fluorite and diamond
dodecahedral - sphalerite

43
Q
A