Exam 1 Flashcards
(36 cards)
Nebula
Collection of dust and gas in space
Nebular Hypothesis
A gravitational pull that creates enuresis that clumps up particles into disks. AKA Accrection.
The Moon
Composition: Similar to Earth’s Mantel
Formated by “The Giant Impact Hypothesis” where an asteroid collided into earth.
The Earth’s Composition
- Core: Nickel & Iron
- Mantel: Peridotite
- Crust: Granite
OCEANIC CRUST: 2.9 G/cm3
CONTINENTAL: 2.7 G/CM3
The Earth’s Physical Properties
- Inner Core: Solid
- Outer Core: liquid
- mesophere: Plastic Characteristics
- Asthenosphere: Plastic; WEAK; Less pressure
- Lithosphere: Solid Rock
DENSITY starts at the core and gets lighter outwards
Alfred Wegener
(1912) German Meterologist, proposed PANGEA aka Plate Tectonics
Plate Tectonics Evidence
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
Covergent Plates
Oceanic crust Vs O.c
Continental crust Vs C.C
O.C Vs. C.C
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
Divergent Plates
C.C Vs C.C
O.C vs. O.C
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
Transform
Plates slide across each other / shear
ex. San Andreas
Wilson Cycle
Divergent 1.Conception.. E african rift 2.Embryonic...Red Sea 3.Juvenile... linear seaway 4. Mature ^^^Divergent^^^ 5.Declining 6.Terminal 7.Suturing ^^^Convergent^^^
How fast do plates move?
Speed depends on pace
Driving force of plate tectonics
- Convection «< MOST IMPORTANT
- Ridge Push
- Slab Pull
- Slab Suction
Stress
Force per unit area
|»_space;> Strain: change in size in response to stress
Rock’s Response to Stress
Elastically: return to shape after stress, deforms permanently after hitting exceeding limit
Ductile: Bending
Brittle: Deformation involves fracturing
Outcrops
bedrock exposed at the surface
Strike-slip Faults
Horizontal direction bedrock runs
Left & Right lateral motions
Dip-slip
Vertical Motion
normal faults- extensions
reverse faults- places older rock on top
Horsts and Grabens- forms when crust stretches apart
Joints
NOT FAULTS
Aseismis- no earthquak hazard
influence- rock stregnth, landslides and slope failure, ground water movement
Earthquake
> p-waves
S-waves
Surface Waves
- Focus
- Epicenter: where energy is first met
- 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
Trans tension
pulls apart and creates a deep basin
transpression
conversion which creates hills and mountains
Measuring Earthquakes
Seismograph
Modified Mercalli
1 to 12; descriptive