Exam Review Flashcards

1
Q

Geology

A

Study of the Characteristics and history of the Earth

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2
Q

Scientific method

A

Method for identifying a problem and coming up with and testing solutions to explain how the physical universe works

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3
Q

Earth’s age

A

4.54 Billion years old

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4
Q

Geologic time

A

million and billions of years

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5
Q

Uniformitarianism

A

The process we see in the Earth today happened in the past

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6
Q

Origin of Universe

A

Big Bang Theory: Explosion and expansion from a singularity

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7
Q

Origin of Solar system

A

Solar Nebula Theory: Rotating cloud of gas collapsed because of a shockwave

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8
Q

Hubble’s Law

A

Galaxies are receding at a velocity proportional to their distance from us

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9
Q

Earth’s Chemical Layers

A

Crust, Mantle, Core

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10
Q

Earth’s physical layers

A
Lithosphere: crust and upper mantle
Asthenosphere: Upper mantle: plasticy
Lower mantle: solid
Outer core: Liquid: Created magnetic field
Inner core: solid
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11
Q

Mineral

A
Naturally occurring
inorganic
Crystalline solid
narrowly defined chemical comp
Characteristic physical properties
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12
Q

Matter

A

substance of which any physical object consists or is composed

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13
Q

Electron structure

A

ring 1 - 2
ring 2 - 8
ring 3 - 8

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14
Q

Ionic bonding

A

Electron is lost or gained and atom becomes an ion
Cation = +
Anion = -

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15
Q

Covalent bonding

A

Atoms share electrons

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16
Q

Metallic bonding

A

Electrons migrate among atoms of other like metals

17
Q

Van der Waals

A

Weak attractive force between neutral atoms3

Only really graphite

18
Q

Isotope

A

Variation in number of neutrons

19
Q

Radioactive decay

A

Atom releases energy to return to natural state

20
Q

Rock forming Mineral

A
(O)ld
(Si)lly
(A)unt
(Fe)y
(C)an
(N)ever
(K)iss
(M)en
21
Q

Silicates

A

Si-O tetrahedron
Dark silicates = Ferromagnesian minerals
Light silicates = Non-Ferromagnesian minerals

22
Q

Non-Silicates

A
Oxides
Sulfides
Sulfates
Halides
Carbonates
Native Elements
23
Q

How minerals form

A
Solidification from a melt (most common)
Precipitation from a solution
Solid state alteration
Biomineralization
Chemical alteration
24
Q

Gemstones

A

Perfect Mineral that has special value

25
Q

Evidence for continential drift

A
Fit of continents
Rock sequence
Mountain ranges
Glacial deposits
Paleoclimates
Fossil correlation
26
Q

20th century evidence

A

Seamount Chains and Fracture zones

Sediment thickness and Age

27
Q

Earth’s magnetic field (magnetosphere)

A

Giant bar magnet. Radiates from south pole and loops to North pole.
Flowing of Iron in outer core generates mangetic field

28
Q

Paleomagnetism

A

Magnetism in rocks

29
Q

Polar wandering

A

Movement of tectonic plates caused magnetic rocks to lead to different locations for amgnetic poles

30
Q

Tectonic plates

A

Continental
Oceanic
Combination

31
Q

Plate boundaries

A
Divergent = Push apart
Convergent = Push together
Transform = Slide past eachother
32
Q

Hot stops and Mantle plumes

A

Intra plate: can happen within the middle of a plate
Deep upwelling from mantle reach crust and start to fracture, creating volcanic island: Hawaiin islands.

Do not move, the plates move.

33
Q

Active margin

A

boundary between two plates

34
Q

Passive margin

A

in the middle of a plate, away from any boundary between plates