Quiz 4 Flashcards
Lithosphere
Consists of the crust and upper mantle
Asthenosphere
The ductile (flexible) portion of the upper mantle
Lithospheric plates…
Move across the asthenosphere
Alfred Wegener
Postulated the theory of continental drift
(Alfred Wegener)
3 forms of evidence:
- Continents fit like a puzzle
- Similar fossils on different continents
- Geological structures
- Paleomagnetism
Ocean-ocean convergence
Oceanic crust –>
Continent-continent convergence
Continental crust –>
Ocean-continent convergence
Oceanic crust –>
Ocean-ocean divergent
- builds mid-ocean ridges, new crusts
Continent-continent divergent
- builds ocean basin
Transform boundaries
- moderate to massive earthquakes
- horizontal movement of two plates in opposite directions
• high friction, high tension
Ex. San Andreas fault, CA
Subduction zone
The oceanic crust usually sinks into the mantle beneath lighter continental crust
Why does oceanic crust subduct under continental crust?
Oceanic crust weighs more and is denser than continental crust
Doctrine of Uniformitarianism
- gaps in geologic record
A. Disconformity
B. Angular unconformity
C. Nonconformity
Principle of Horizontality
| | | | | v v v v v 3 limestone | 2 | sequence of events 1 sandstone V Undisturbed layer
Law of Superposition
Rank of age of the rock layers from oldest to youngest
1>2>3
Oldest–>youngest
Principle of Inclusions
Inclusions: physical evidence in the disturbed rock layer
Ex. Of disturbance includes erosion, uplifting by subterranean forces, folding, faulting, etc…
REMEMBER- Inclusions are older than the rock that contains them
Principle of cross-cutting relationships
Bottom line - when an intrusion or fault cuts them an existing feature, it is the youngest event
Principle of fossil succession
If we know the kind of fossil, preserved in the rock layers, the relative age of the rock can be determined
Absolute dating
Numerical age - use radiometric dating technique
• half life: the amount of the time it takes for half the parent radioactive element to decay to a daughter period
Wavelength
Distance between two successive crests
Wave period
Time between two successive crests
Wave crest
Highest point of a wave
Wave trough
Lowest point on a wave