džiomorfolodži Flashcards
(45 cards)
Layers (4)
Crust
Mantle
Outer & Inner Core
Lithosphere
Crust + Upper part of Mantle
Asthenosphere
Part of upper Mantle below Lithosphere
Flows like molten plastic despite being solid
Outer Core
Fluid layer of Earth’s Core
Primarily composed of Liquid Iron & Nickel
4500C to 5500C
2900km to 5100km
Inner Core
5100km to 6371km from surface
Probably: solid, composed by iron-nickel alloy
->deduced from seismic waves & magnetic field
Tectonic plates boundaries (3)
Divergent, Convergent, Transform
Divergent boundary - Separation
Plates move away from each other
New crust
Under oceans usually (basalt)
Mid-Atlantic Ridge
East African Rift Valley
Constructive
Convergent boundary - collision
Causes: Subduction OR Collision
Creates mountains
Subduction - usually oceanic going under continental
Destructive
Transform (Sliding)
Plates slide past each other horizontally
Causes Earthquakes
E.g.: San Andreas Fault
Convergent - results
Mountains, Trenches, Volcanoes
Divergent - results
Ridges, Valleys
Transform - results
Earthquakes, faults
Fault
Break or fracture of Earth’s crust where rocks have moved past each other
Cause: tectonics forces that are too strong, causing rocks to crack and shift
Result: Displacement: up/down/sideways
Mohorovicic Discontinuity/Moho
Seismic waves change speed as they move
Speeding up when pass through bottom of crust enter mantle
Boundary between crust and upper mantle
Desulforudis Audaxviator
Species of bacterium that lives in groundwater 1.5-3km below Earth’s surface
Jules Verne’s novel Journey to the Center of the Earth: “Descende, audax viator, et terrestre centrum attinges”
Magnetic Motion
Earth’s north magnetic pole is moving away from Canada toward Siberia
Folds
Bend in rock layers caused by slow compression
Cause: Rock layers are soft/flexible, pressure applied slowly, so they bend instead of breaking
Result: Curved structures: Anticlines(upfolds)/Synclines(downfolds)
Convection Currents
Circular movements of material caused by differences in temperature/density in Earth’s mantle
Convection Current process (technically 4 but 5)
- Heat from Core warms lower mantle
- Hot mantle material becomes less dense and ascends
- Reaching cooler upper mantle makes it spread out and cool down
- Cooler and denser material sinks back toward lower mantle
- Cycle…
Mantle Plume
- Narrow column of hot rock that rises deep within the mantle, possibly near Core
- Hotter & more buoyant than surroundings, causing it to rise vertically and drastically
- When it reaches lithosphere, it can cause volcanic activity(e.g. Hawaii Islands formed over a mantle plume - hot spot)
Hot Spot
Usually away from boundaries
Caused by Mantle Plumes
Ring of Fire
Location: Around Pacific Plate edges
Cause: Convergent plate boundary = Subduction
Definition: Zone of intense volcanic and earthquake activity
Continental crust
thicker/stronger 35-40km
older
less dense
mostly granite
Oceanic crust
slightly denser
much thinner 5-10km
younger
mostly basalt