exam 1 Flashcards

(69 cards)

1
Q

radius of the earth

A

4000 miles

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2
Q

circumference of the earth

A

2500 miles

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3
Q

revolution

A

1 year, noncircular elliptical orbit

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4
Q

distance from earth to sun

A

93 million miles

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5
Q

phase of revolution where the earth is farther away from the sun

A

aphelion, 93 million miles

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6
Q

phase of revolution where the earth is closer to the sun

A

perihelion 91 million miles

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7
Q

amount of years it takes for the orbit of revolution to rotate 360 degrees

A

100,000 years

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8
Q

rotation time and speed

A

1 day, 1000 mph

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9
Q

earth shape created by the forces of gravity causing expansion at the equator

A

oblate spheroid

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10
Q

study of the shape of the earth

A

geodisy

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11
Q

tilt of the earth causing seasons

A

axial tilt, 22-24.5 degrees

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12
Q

amount of time it takes for the axial tilt to change from one extreme to another and back

A

40,000 years

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13
Q

wobble of the axis of rotation

A

precession, full one takes 26,000 years

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14
Q

cycles that map out the occurrence of each of earth’s motion cycles to determine when they will coincide potentially causing weather extremes like the ice age

A

Milankovitch cycles

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15
Q

created by the earth’s rotation and core rich in iron; acts as a shield protecting the earth from the sun’s harmful rays

A

magnetic field

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16
Q

prior to 1780, school of thought that the earth was formed by a series of infrequent major events such as volcanos and biblical floods

A

catastrophism

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17
Q

post 1780, school of thought that the earth was shaped by frequent minor events over a long period of time such as rivers, wind, and tectonic shifts

A

uniformitarianism

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18
Q

location and person who discovered evidence of uniformitarianism with shifts in the rocks, caused the shift from catastrophism to uniformitarianism

A

Siccar point Scotland, James Hutton, 1780

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19
Q

location and person who recognized large land ripples similar to that of sand likely caused by catastrophic floods leading to the proposal of neo catastrophism

A

J Harlan Bretz, Channeled Scablands, Washington state, 1920s

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20
Q

modern school of thought that uniformitarianism and catastrophism work in conjunction to shape the earth

A

neo-catastrophism

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21
Q

law that states the oldest rocks are found on the bottom and the newest on the top

A

law of superposition

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22
Q

law that states sediments that became rocks were originally laid down horizontally, some remain that way but some shift

A

law of original horizontality

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23
Q

size order for sections of the geologic time scale

A

Eon>Era>period>epoch

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24
Q

now the geologic time scale was Originally made

A

relative age dating based on floral and faunal succession

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25
recent technology allows for this type of dating using radio active elements discovered in 1960'5 by marie curie
absolute age dating
26
decay of radioactive isotopes over time allows for this method bused on the energy they emit as a parent decays into the daughter
half like decay
27
Oldest Object we have dating to 4.3 bya found in Jack hills of western australia
Zircon crystal
28
Earth begins
4.6 bya
29
2.5 bya divide proterozoic and archeon marked by this event made obvious by the presence of rust in fossilized rocks
great oxidation event
30
541 mya paleozoic begins with this event marked by the appearance of fossil hard parts
cambrian explosion
31
mesozoic begins marked by major reptiles
252 mya
32
66 mya this event marks the end of the mesozoic
KT extinction
33
KT boundary is rich in this element indicating an asteroid
iridium
34
Pleistocene begins with continental glaciation starting the quaternary period
2:6 mya
35
mup of largest known glaciers 18,000 ybp causing a rapid 400 ft rise in sea level upon melting
glacial max
36
Pleistocene ends win a full meltdown starting the holocene
10,000 ybp
37
age of rocks on Ship campus
ordovician ,490 myo
38
number of naturally occuring elements
88
39
% of the earth's crust made of the most abundant 8 elements
98.5 %
40
most abundant 8 elements
oxygen silicon aluminum iron calcium sodium potassium magnesium
41
Incredibly inert chemical formula that makes up quartz
silica siO2
42
chemical formula that makes up the earth's crust
SiAl silica + Al
43
mafic
Mg+ Fe
44
makes up oceanic crust
sima silica + ma fic
45
number of recognized minerals
5,500
46
naturally occuring inorgan. solids with a definite chemical structure and a unique set of physical properties
Minerals
47
most obvious and least Reliable physical property
color
48
physical property refering to now light is reflected, metalic
luster
49
measured by the mons scale where diamond is a 10 and talc is a 1
hardness
50
physical property of the color of a Minerals powder
streak
51
physical property of now light is transmitted through a mineral
Diaphaneity
52
melting or crystallizing point range
800 - 1200 C
53
most reliable and least obvious physical property bused on the number of visible geometric planes when a mineral breaks
Cleavage planes
54
3 cleavage planes
cubic
55
4 cleavage planes
pyramidal
56
how a mineral grows
habit
57
iron ore metalic gray with red streak I plane of cleavage that can't be seen
hematite
58
no cleavage, harder than glass
Quartz
59
4 cleavage planes softer than glass
fluorite
60
metalic silver with cubic Cleavage and high density
galena
61
feldspar with strianons and irridesence
plagiocIase
62
feldspar without strations
potassium
63
olive green With no Cleavage planes, melts at 1200 c
Olivine
64
one plane of cleavage sheet like and transparent
muscovite
65
softer than a fingernail 0 Cleavage planes
Kaolinite
66
fool's gold metallic with 0 planes of Cleavage but Cube habit
pyrite
67
rhombohedralCubik cleavage reacts with HCI
calcite
68
Cubic Clearage greasy feeling transparent
halite
69
60-120 cleavage on 2 planes
Hornblende