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
Oceanic-continental convergent boundary
* 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
Continental-continental convergent boundary
* 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
Transform
* plates slide laterally (sideways) past each other along faults * these boundaries change one type of motion between plates into another type of motion
28
Hot spots
* 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
Mantle plumes
* remain stationary * while plates move over them, trail of extinct and progressively older volcanoes that record the movement of the plate is left
30
Mineral deposits
* many of the world’s major metallic ore deposits are associated with convergent and divergent plate boundaries * hydrothermal activity, often volcanic
31
Continental accretion
* process of adding material to a continent * common along convergent oceanic-continental plate boundaries
32
Mineral
* natural * inorganic * crystalline solid * characteristic physical properties * specific chemical composition
33
Most common minerals are made up of ___, ___, and one or more other elements.
oxygen, silicon
34
Silicate minerals
composed of the silica tetrahedra most minerals are silicates (compounds of silicon and oxygen, and other elements)
35
Ferromagnesian silicates
made up of iron and or magnesium, combined with other elements dark in color and dense olivine and biotite
36
Non-ferromagnesian silicates
lack iron and magnesium light colored
37
Carbonate minerals
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
Native elements
composed of a single element gold, copper and diamonds
39
Sulfide minerals
contain sulfur plus a metallic element as in galena (PbS) and pyrite (FeS²) commonly form along mid-oceanic ridges
40
Sulfates
have the sulfate radical (SO4 -²) as in gypsum (CaSO4 2H2O) common in deserts, forming from evaporation of water
41
Mineral cleavage
refers to the breakage or splitting of mineral crystals along one or more smooth planes determined by atomic structure
42
Number of cleavages and direction 1 2 at right angles 3 at right angles 3 at not right angles 4 6
Cleavage name micas (biotite) prismatic - feldspars cubic - halite and galena rhombohedral - calcite and dolomite octhahedral - fluorite and diamond dodecahedral - sphalerite
43