Lab Exam 2 Flashcards

1
Q

If you were to cut earth in half from a side view what would you see in terms of layers

A

Ocean, oceanic crust seperating the ocean floor and the Lithosphere, then under the lithosphere is the Asthenosphere.

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2
Q

Where the ocean meets land is called what

A

continental crust

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3
Q

What rocks are the most and least dense

A

most dense: Asthenosphere

Least Dense: Continental crust

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4
Q

Isostasy

A

geologic term that describes the effects of gravity on the Earth’s crustal plates.

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5
Q

isostatic equilibrium

A

gravitational force pulling them down is offset by buoyancy of the rocks in the crust.

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6
Q

Density Equation

A

mass/Volume

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7
Q

Coasts can be divided into two types:

A

active margins and passive margin

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8
Q

Active margins

A

are found where subduction occurs along the edge of the continent

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9
Q

passive margins

A

found along tectonically-quiet coastlines.

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10
Q

continental shelf

A

part of the continent which has been flooded by the ocean, and commonly sediments accumulate on the shelf.

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11
Q

continental slope

A

transition between continental crust and ocean crust

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12
Q

abyssal plain

A

the deep, flat parts of the ocean basins, and they account for over half of the Earth’s total surface area.

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13
Q

volcanic island arc

A

forms if subduction is occurring between two oceanic plates

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14
Q

continental volcanic arc

A

forms if an oceanic plate is subducting under the edge of a continent

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15
Q

Phaneritic rock

A

Coarse-Grain

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16
Q

Aphanitic Rock

A

Fine-Grain

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17
Q

Half-lives =

A

ln (z) • (-1.4426) where z = parent ratio

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18
Q

Parent Ratio

A

Parent Amount/(Parent+Daughter)

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19
Q

Original Material:

A

As it implies, this type of fossil is one composed of original material. This can include soft tissues such as hair, skin or organs, and hard materials such as bone (phosphate), shells (carbonate)

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20
Q

Replacement

A

In this type of fossilization, the original organic material is replaced by another mineral.

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21
Q

Permineralization:

A

As fossilization progresses, empty spaces in the original fossil can become filled in with minerals

22
Q

Carbonization:

A

In some instances, the original organism is flattened out into a thin film of black or brown carbon.

23
Q

Mold and Cast:

A

When an organism is buried, an imprint of the fossil will form a “mold” in the sediment surrounding it

24
Q

Magnitude =

A

Log (H) - Log (A )
Where H = height of the biggest S-wave in mm.
Log (A ) is determined using the distances

25
Q

Porosity

A

measure of how much empty space a rock contains relative to the total volume of the rock

26
Q

Permeability

A

a measure of how well connected the pore spaces are. The higher the permeability, the easier it is for water to move through the rock

27
Q

aquifers

A

Bodies of rock with good porosity and good permeability (“sponges”)

28
Q

Unconfined aquifers

A

are the bodies of rock nearest the Earth’s surface and they are fed by water infiltrating in from directly above

29
Q

Confined aquifers

A

are aquifers which are not recharged directly from the land surface above. Instead, water enters the aquifer in a recharge area at some other location, sometimes thousands of miles away.

30
Q

aquitards

A

bodies of rock with poor porosity or poor permeability (or both)

31
Q

four types of stream channels

A

Straight, Meandering, Braided, anabranching

32
Q

Straight channels

A

can occur but they are rare, literally straight

33
Q

meandering pattern

A

display a sinuous or snake-like pattern as they flow across the land surface (most common)

34
Q

braided channels

A

have numerous braid bars which are constantly changing and shifting over time

35
Q

anabranching channel

A

braid bars may become stable, permanent islands, forming these types of channels

36
Q

Salinity Equation

A

Salt+Water

37
Q

Shallow water wave wave depth equation

A

Water depth = 1/20 * wavelength

38
Q

Deep water wave wave depth equation

A

Water depth = 1/2 * wavelength

39
Q

wave refraction

A

waves approaching shore get bent (refracted), causing the wave energy to be focused on the headlands and away from the embayments

40
Q

Specific Gravity/ Cleavage

A

the the number of sides and divide by 2 to get the number of cleavage.

41
Q

Mafic Rock

A

dark in color

42
Q

Intermediate Rock

A

Salt and pepper look

43
Q

Felsic Rock

A

white, light grey or pink in color

44
Q

Clastic vs. Chemical rock

A

Chemical rock looks more crystalized while clastic rock looks more dull.

45
Q

Banded, Foliated, and non-foliated rock

A

Banded is minerals in distinct bands
Foliated is literal layers like pieces of paper
non foliated is no pattern, kinda crystalized

46
Q

Gastropods

A

snail shell, coiled shell

47
Q

Bivalves

A

stereotypical shell, oyster shell or seashell

48
Q

Cephalopods

A

swirly and look like an octopus tentacles

49
Q

Brachiopods

A

look much like regular seashells but are Symmetrical from the top view

50
Q

Trilobites

A

exoskelton of an arthropoda, like a dank fossil