Lecture 14 Flashcards

1
Q

What are the major zones of the earth?

A
  • Crust
  • Mantle
  • Core
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2
Q

Mineral

A

A naturally occuring, inorganic, element or compound, with a definite internal arrangement of ions(solid) and a chemical composition that is fixed or varies within narrow limits.

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3
Q

Rock

A

Aggregates of one or more minerals, found on earth’s crust.

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4
Q

What is the most abundant mineral in earth’s crust?

A

Oxygen

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5
Q

How can oxygen be part of the crust?

A

Very reactive, so reacts with other elements

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6
Q

Native elements

A

Pure elements

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7
Q

What are the most abundant mineral groups?

A

Silicates

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8
Q

When is the chemical make up of minerals more common?

A

In ion substitution

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9
Q

What are the ways to identify minerals?

A
  • Hardness
  • Color, luster, streak
  • Density
  • Cleavage/fracture
  • Magnetic properties
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10
Q

silica tetrahedron

A

Silicon atom attached to four oxygen atoms by tetrahedral bonds, results in a 4- charge on the SiO4 (silicate) group. Basic building block of silicates.

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11
Q

Pyroxenes

A

Single chains of tetrahedra balanced by similar metal cations and sodium(Na)

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12
Q

Amphiboles

A

Double chains of tetrahedra balanced by similar cations.

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13
Q

Micas and Clay materials

A

Sheets of tetrahedra are the building blocks. Aluminum is also involved in these sheet structures which are charge balanced by the cations Mg, Na and K

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14
Q

Feldspars

A

A second group of alumino-silicates, the tetrahedra form three-dimensional frameworks with Ca, Na and K as the balancing cations.

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15
Q

Quartz

A

Three dimensional framework structure without cations an just silica tetrahedra. Very stable

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16
Q

What are mineraloids?

A

Not minerals include Opal and amber

17
Q

How are minerals formed?

A

Formed by crystallization. The center of the earth causes rocks to melt forming magma. When magma cools various elements and ions come together to form very specific structure. Different minerals form at different temperatures.

18
Q

What are the three categories of rocks?

A

Igneous, Sedimentary and Metamorphic

19
Q

Igneous rock

A

formed by the crystilization of magma. Two forms:

1) Extrusive(volcanic)-rapid cooling, usually derived from upper mantle high quantities of iron and magnesium
2) Intrusive(plutonic)-slowly cooling, usually derived from crust so relatively rich in silicates and aluminum.

20
Q

Sedimentary rock

A

formed by the sedimentation and campaction of material(lithification)
-tends to form in layers

21
Q

Metamorphic rock

A

Rock that has been chemically altered while in the solid state from exposure to high temperatures and pressures. The process is re-crystallization

22
Q

Rock cycle

A

Goes from igneous to sedimentary to metamorphic and back to igneous. Look at slide photo

23
Q

What are the parts of the earth’s core?

A

inner (solid) core

outer (liquid) core

24
Q

Seismograph

A

Measures and records the minute tremors of the earth

25
Q

How have the properties of the inner earth been analyzed?

A

Looking at meteorites(similar in composition to earth) and the seismograph

26
Q

What are the two waves propogated by the earth?

A

Surface waves(travel along the surface) and Body Waves(travel on earth interior)

27
Q

What are the forms of body waves?

A

P-waves and S-waves

28
Q

P-waves(primary waves)

A

compression waves like sound waves

29
Q

S-waves(secondary or shear waves)

A

Involve displacement perpendicular to the direction of the wave.

30
Q

What body wave type is fastest?

A

P-waves

31
Q

The S Shadow

A

S-waves do not propogate through the liquid outer core. Since S-waves only travel through solid material, it has been concluded that the outer core must be composed of molten metals.

32
Q

Does the earth interior have an effect on wave velocity?

A

Yes, changes in the properties of the earth interior with depth cause the waves to bend.

33
Q

lithosphere

A

composes the first 70-125km of the solid earth, consists of the oceanic and continental crustal material plus the uppermost portion of the mantle. It is rigid and acts as a single unit.

34
Q

asthenosphere

A

(~100km in depth) characterized by low p-wave velocities. Because of low velocities geologists have deduced that the layer is plastic(not liquid or solid) as a result provides.

  • source of material ejected in volcanoes
  • rebound of crust following ice ages
  • provides malleable layer upon which plates can flow