Exam Review Flashcards

1
Q

What were the 4 basic forces that separated out during the Big Bang?

A
  1. Gravity (attraction of bodies)
  2. Electromagnetic force (electricity & magnetism)
  3. Strong Magnetic Force (hold neutrons and protons together)
  4. Weak magnetic force (breakdown of atoms=radioactive decay)
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2
Q

What are the 5 characteristics of a mineral?

A
  1. Naturally occurring
  2. Inorganic (not living)
  3. Crystalline solid
  4. Defined chemical composition
  5. Characteristic physical properties
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3
Q

4 types of Bonds?

A
  1. Ionic: chemical bonding attraction between 2 ions of opposite charge
  2. Covalent: the sharing of e- between atoms
  3. Metallic: extreme e- sharing. E- of the outer most electron shell easily move from one atom to another
  4. Van der Waals: (residual bond) Weak attractive force when no e- are available
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4
Q

What limits the amounts of minerals (3,500) that exist?

A

Many combinations of elements simply don’t occur. Bulk of earths crust is made up of only 8 chemical elements

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5
Q

Difference between ferromagnesian and non-ferromagnesian silicate minerals?

A

Ferromagnesian contains iron, magnesium or both and is usually darker and dense. Non-ferromagnesian does not contain iron or magnesium and is light colored and less dense.

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6
Q

2 major ways minerals form

A

Form out of a solution. Crystallization of magma or lava

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7
Q

2 sources for magma

A

Crust: more silica rich.

Upper mantle: less silica, more ferromagnesian silicates

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8
Q

How are magmas classified?

A

Magmas are classified according to how much Si they contain

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9
Q

Viscosity:

A

A liquids resistance to flow

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10
Q

High viscosity:

A

all natural peanut butter (flows slow/not very easily)

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11
Q

Low viscosity:

A

honey (flows faster/smoother)

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12
Q

What changes the composition of magma?

A

Crystal settling: physical separation of minerals by crystallization and settling.
Assimilation: magma reacts with country rock

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13
Q

What are Plutons?

A

An intrusive igneous body that forms when magma cools and crystallizes within the crust.

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14
Q

Volcanism:

A

Process by which magma rises and issues onto Earth’s crust.

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15
Q

What are the names of the two common lava flows? What’s the difference between the 2

A

Pahoehoe: Ropy surface like taffy, less viscous
Aa: Jagged and angular, more vicsous

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16
Q

Volcanoes:

A

Classified by eruption characteristics as either quiet vs. explosive.

17
Q

Quiet Volcanoes

A

Low silica percentage = mafic rocks = flow faster = smoothers, more fluid and not as eruptive

18
Q

Explosive Volcanoes:

A

High silica percentage = felsic rocks = flow very slow, eruptive, thick

19
Q

What are the two types of sediment?

A

Detrital: solid particles from preexisting rocks
Chemical: minerals that precipitate from solutions and minerals derived from water by organisms to build shells (biochemical sediments)

20
Q

What are the 5 types of weathering?

A
  1. Frost Actions
  2. Pressure Release
  3. Thermal Expansion/Contraction
  4. Salt Crystal Growth
  5. Living Organisms.
21
Q

3 types of metamorphism and how they differ?

A
  1. Contact (thermal) metamorphism
  2. Dynamic metamorphism
  3. Regional metamorphism
22
Q

Agents of Metamorphism?

A
  1. Heat: Increases rates of chemical reactions
  2. Pressure: Pressure increases with depth
  3. Fluid activity: Water (and carbon dioxide) are present in almost every region of metamorphism
23
Q

What does metamorphic grade mean?

A

the degree to which a rock has undergone metamorphic change

24
Q

Foliated texture

A

Platy and elongate minerals aligned in a parallel fashion

25
Q

Nonfoliated texture:

A

no discernable preferred orientation of minerals. Contact or regional metamorphism of rocks with no platy or elongate minerals

26
Q

Metamorphism

A

the phenomenon of changing rocks subjected to heat, pressure, and fluids so that they are in equilibrium with a new set of environmental conditions

27
Q

What is Parent material

A

rocks acted on by weathering

28
Q

What is Weathering?

A

the physical breakdown and chemical alteration of rocks and minerals at or near the Earth’s surface

29
Q

Chemical weathering

A

decomposition of rocks by chemical alteration of parent material (plants, algae, acid rain)

30
Q

How are detrital sedimentary rocks classified?

A

Classified by size of particles

31
Q

What are the soil formation factors and which is most important?

A

Climate most important
Temperature
Precipitation
Varies by latitude, affects vegetation • Rock type can have some control

32
Q

What is soil? What does it consist of (it’s composition)?

A
  • Humus: microorganisms decompose leaf and grass litter – Release nutrients into soil
  • Burrowing animals mix soils and create channels for air and water
33
Q

Ways in which soil is degraded?

A
  • Any process that leads to loss of soil productivity
  • Erosion: natural process that humans accelerate (plowing, overgrazing, deforestation)
  • Erosion from running water:
  • Nutrient depletion from intensive agriculture • Salinization: increased salts in soil
  • Contamination with toxic substances
  • Compacted soils
34
Q

Mechanical Weathering?

A
  • disaggregation of rocks by physical processes that creates smaller pieces that retain parent composition