-
Types of Deformation
- 1.) elastic deformation – rock will return to original size & shape after the force is removed.
- (Elastic limit – point at which a rock breaks)
2.) brittle deformation – rock breaks
3.) ductile deformation – rock bends and doesn’t return to original shape when the force is removed.
-
Types of Stress (Force acting upon a rock)
- Ithostatic (confining) presssure– equal in all directions;
- changes size, not shape
differential stress – not equal in all directions
- compressional stress –pushing together
- -shortens & thickens crust
- -at convergent plate boundaries
- tensional stress – pulling apart
- -lengthens & thins crust
- -at divergent plate boundaries
- shear stress – parallel; forces in opposite directions
- -at transform & convergent
- -plate boundaries
-
Orogeny
Mountain building event
-
Angle of Repose
Steepest angle of which unconsolidated material is stable
-
How is Mass Movement Classified?
Type of material
Type of motion
Velocity
-
Ore
Rock that contains a desired material in concentrations economic to extract
-
Liquefaction
- Occurs in water saturated sediments
- -amplifies vibrations
- -sinks structures
-
How is a Tsunami generated in an earthquake?
Underwater EQ moves the seafloor up at a fault, pushing water up before it crashes down
-
Epicentre
Point on Earths surface, directly above the focus
-
Focus
First movement on a fault (where earthquake begins)
-
Primary Wave
(P Wave)
Body Wave (travels through earth)
- Compressional "push & pull" motion
- Fastest waves
-
Secondary Waves
(S Waves)
Body Wave (travels through earth)
- Shear "side to side" motion
- Always slower than P Waves
- Cannot travel through liquids
-
Rayleigh Waves
-Surface Wave: travels along earths surface
Up-and-down movement
-
Love Waves
-Surface Wave: travels along earths surface
Side to side movement
-
How does a Seismograph work
Works through inertia (ground moves under an object that wants to stay at rest)
-
What is Modified Mercalli Index? Why is it useful to scientist?
- Measures intensity (degree of shaking)
- Helps us see how the damage can vary from one earthquake to another
-
Isostasy
Crust floating in gravitational balance
-
Pegmatites?
- Last part of an igneous intrusion to cool
- Can be enriched in incompatible elements
-
Kimberlites?
- Volcanic pipe from the mantle
- Ex. Diamond
-
Resources
Total amount of a geologic material in all deposits, discovered and undiscovered
-
Reserves
Discovered resources that are economic to extract under conditions such as economics, technology, and politics
-
Shield (of continent)
Old original part of continent
-
Basement (of continent)
Older metamorphic & intrusive igneous rocks upon which younger sediments rest
-
Terrane
Crustal block with a different history than surrounding blocks
-
Different grades of coal are?
- Peat
- Lignite
- Bitumunous
- Anthracite
-
Four things you need to have an oil deposit are?
- Source Rock-organic rich shale
- Must pass through oil window
- Reservoir Rock-good porosity & good permeability
- Trap-impermeable
-
Oil Window
Conditions (temperature) needed to make oil
-
What causes Hydrothermal mineral deposits?
Hot water circulating through rock
-
Vein Deposit
Tabular body of minerals deposited in a crack
-
Disseminated Deposit
minerals scattered along tiny cracks in a large volume of rock, extracted by open pit mines
-
-
-
Fold & Thrust Mountains form in?
continent-continent collision environments
-
How do fault block mountains form?
by movement on normal faults
|
|