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Chezka Llanera
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Science
General science
198 cards
Cards (364)
Planet
earth
34.6
% Iron
29.5%
Oxygen
15.2
% Silicon
12.7
%Magnesium
Axis
23.5
tilted
Rotation
24
hours
Revolution
365
dqys
1/4
Leap year
366
days
Equilateral
Radius 6378
Polar
radius 6357
Equilateral
Circukference
40076
Polar
circumference 40008
Volume
26000000000 mi3
Density
5.52
Crust
Outermost layer of the arth
Continental
Sial
Oceqnic
Sima
Lithosphere
Enture crust and uppermost mantle and forms earth relatively cool,rigid outer shell
Asthenosphere
Soft,comparatively weak layer beneath the lithosphere
Mantle
Semi-molten iron and magnesium silicater layer that makes up 80 % eaths volume
Mesosphere
Lower mantle,solid,rocky layer
Core
Innermost and densest layer of the earth
Outer
core
Molten Metallic layer
Inner
core
Solid iron part due to immense pressure
Mohorovicic
Between crust and mantle
Gutenberg
Between mantle and core
Lehmann
Between outer core and inner core
Continental
Drift
theory
Proposed by Alfred Wegener
Pangaea
Supercontinent
Panthalassa
Single vast ocean by pangaea
Laurasia
Northern part
Gondwanaland
Sothern part
Plate
tectonics
States the earth rigid outershells
Lithospheric plates
Broken into numerous slabs,continual motion
Transform
Slide past each other
Convergent
Plates move towards each other
Divergent
plates move apart
Sea-floor
spreading
Features of the oceqn floor and why drifting of continents take place
Earthquake
Shaking of the ground by the sudden breaking and shifting of large secfions
Focus
Origin of the earthquake
Epicenter
Point in the surface directly above the focus
Faults
Break in a rock mass
Normal
fault
Hanging wall moves down,divergent boundarues
Reverse
fault
Convergent boundaries
Strije slip
fault
Side by side sliding movement
Tension
forces
Strech rock layers from opposite directions,rock layers pulled apart
Compression
forces
Push rock layers from opposite sides
Shearing forces
Pull rock layers in different directions
Tsunami
Large destructive waves caused by an earthquake
Seismic
waves
Waves of energy result low frequency acoustic energy
Body
waves
Travel throughs the earth interior
Primary waves
Displaced parallel to the direction of the wave, can travel through solid and liquid
Secondary waves
Displaced perpendicular to the direction of the wave can travel through liquid
Surfaces
waves
Travel along earths surface
Love wave
Fastest surface wave and move the ground from side to side
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