Exam 1 Flashcards

(36 cards)

1
Q

Nebula

A

Collection of dust and gas in space

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2
Q

Nebular Hypothesis

A

A gravitational pull that creates enuresis that clumps up particles into disks. AKA Accrection.

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3
Q

The Moon

A

Composition: Similar to Earth’s Mantel

Formated by “The Giant Impact Hypothesis” where an asteroid collided into earth.

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4
Q

The Earth’s Composition

A
  1. Core: Nickel & Iron
  2. Mantel: Peridotite
  3. Crust: Granite

OCEANIC CRUST: 2.9 G/cm3
CONTINENTAL: 2.7 G/CM3

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5
Q

The Earth’s Physical Properties

A
  1. Inner Core: Solid
  2. Outer Core: liquid
  3. mesophere: Plastic Characteristics
  4. Asthenosphere: Plastic; WEAK; Less pressure
  5. Lithosphere: Solid Rock

DENSITY starts at the core and gets lighter outwards

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6
Q

Alfred Wegener

A

(1912) German Meterologist, proposed PANGEA aka Plate Tectonics

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7
Q

Plate Tectonics Evidence

A

1.Fit of Continents
2. Location of the same extinct animal species
3. Location of the same kinds of rocks
4. Past glaciation
MODERN LINES
5.Seismin evidence- Earthquak maps
6.Structural evidence- ridges & trenches
7.magnetic evidence- Strips on seafloor
8.Age of the Seafloor
9.Presence of hot spots- heat builds up @ core-mantel boundary

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8
Q

Covergent Plates
Oceanic crust Vs O.c
Continental crust Vs C.C
O.C Vs. C.C

A

Coming together/ compressing
O.C Vs. O.C : Trenches, subduction zones
C.C Vs. C.C: High Mountains Ex. Himilayas
O.C Vs. C.C: Volcanoes

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9
Q

Divergent Plates
C.C Vs C.C
O.C vs. O.C

A

Going apart / tension
Wilsons cycles: opening & closing of ocean basins
C.C v C.C: Rift valleys
ex. East African Rift
O.C v O.C: Constructive; magma to create new crust
ex. Red Seas

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10
Q

Transform

A

Plates slide across each other / shear

ex. San Andreas

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11
Q

Wilson Cycle

A
Divergent
1.Conception.. E african rift
2.Embryonic...Red Sea
3.Juvenile... linear seaway
4. Mature
^^^Divergent^^^
5.Declining
6.Terminal
7.Suturing
^^^Convergent^^^
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12
Q

How fast do plates move?

A

Speed depends on pace

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13
Q

Driving force of plate tectonics

A
  1. Convection «< MOST IMPORTANT
  2. Ridge Push
  3. Slab Pull
  4. Slab Suction
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14
Q

Stress

A

Force per unit area

|&raquo_space;> Strain: change in size in response to stress

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15
Q

Rock’s Response to Stress

A

Elastically: return to shape after stress, deforms permanently after hitting exceeding limit
Ductile: Bending
Brittle: Deformation involves fracturing

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16
Q

Outcrops

A

bedrock exposed at the surface

17
Q

Strike-slip Faults

A

Horizontal direction bedrock runs

Left & Right lateral motions

18
Q

Dip-slip

A

Vertical Motion
normal faults- extensions
reverse faults- places older rock on top
Horsts and Grabens- forms when crust stretches apart

19
Q

Joints

A

NOT FAULTS
Aseismis- no earthquak hazard
influence- rock stregnth, landslides and slope failure, ground water movement

20
Q

Earthquake

> p-waves
S-waves
Surface Waves

A
  1. Focus
  2. Epicenter: where energy is first met
  3. Fault: Crust Ruptures

P-waves: Primary, compressional, 6km/sec through solids & liquids
S-waves: Secondary, shear, 3km/sec only through solid
Surface Waves:
Love Waves & Rayleigh Waves: Retrograde motion

21
Q

Trans tension

A

pulls apart and creates a deep basin

22
Q

transpression

A

conversion which creates hills and mountains

23
Q

Measuring Earthquakes

24
Q

Modified Mercalli

A

1 to 12; descriptive

25
Richter Scale
measures energy real eased (joules), distance and amplitude
26
Moment Magnitude
Modifies RICHTER, all motion, adds +1 to magnitude, science purposes. -Releases energy over 100s of kilometers
27
Intensity Vs Magnitude
Intensity: How strong it feels towards observers Magnitude: 1.Related to Energy realease 2.determined from seismic records
28
Earthquake predictors
Historical: 1. historical records 2. paleoseismology Short-term: 1.Precursors Long-term Prediction: 1.seismic gaps
29
Lisbon, Portugal (1755)
1. First scientifically studied | 2. Tsunami & Earthquake connections
30
Other important earthquakes
- New Madrid, Missouri (1811-1812) - Tokyo (1923) - Alaska (1964) - Tangchan, China (1976) - Indian Ocean (2004)
31
Charsleton, South Carolina (1886)
First Widely Known u.s earthquake
32
San Francisco (1906)
1st revealed importance of faults
33
Government Regulations
Field Act, Uniform building code, Alquist-Priolo Earthwuak within 50 ft, hospital safety act, dam safety act, and unreinforced masonry building law
34
Earthquake Hazards
Natural: - ground rupturing - shaking - liquification - landslides Handmade: - fire - structure collapse - utlity outage
35
Safest Buildings >> Most dangerous
( 1 safest- 4 most dangerous) 1. Small, wood framed house 2. Steel frame 3. Reinforsed masonry 4. Adobe
36
Base isolation
Isolating the building from the ground using larger rubber rings allow the building to stay stationary while the ground moves