Plate Tectonics Flashcards
Lecture 4
Density
density = mass/volume
if two substances of different densities come into contact and one is acting as a fluid, the substance with lesser density will float above the substance with greater density
tectonic plates vs plate tectonics
TP - large subdivisions in the crust of the planet
PT - the study of the movement of TP
Faults
major fracture in the continuity of two regions of rocks
all plate boundaries associated with faults but not all faults are associated with plate boundaries
Oceanic Crust
density heavier than continental (2.9 - 3g/cm cubed)
uniform thickness
relatively young
mainly found oceans, but not always!
Continental crust
lighter density than ocean crust
differences in thickness - very thick
varying ages - older than oceanic crust
generally found out of water, Zealandia continental crust below ocean)
cratons - oldest and most stable regions of continental crust
Asthenosphere
below upper mantle and crust
hot enough that rock behaves like liquid
How do tectonic plates move?
convection current = movement of liquid rock is driven by in temp. and density btwn outer and inner layers of mantle
Push-pull process
Ridges - creation of new plates where magma rises
Subduction zones - Destruction of plates by crushing (pull down)
slab pull - entire plate pulled by the weight of its cold, dense sub ducting section
Divergent boundary
seafloor spreading - process of tectonic plates moving apart at divergent boundaries, ridges
(where hot liquid rises from the asthenosphere)
brand new crust is hotter, less dense than then older, cooler crust – sinks!
Hydrothermal Sea Vents
weak point in the sea floor where water and minerals heated geothermally enter the ocean, found at divergent boundaries
Rift Valley
When divergent boundary can form on continental crust
rock formed here similar to oceanic crust, denser
eventually all rift valleys will be submerged under water
How can we tell Magnetic Pole Reversals?
when lava rock solidifies, minerals which are magnetized in the rock lock into an orientation reflecting the existing direction of the magnetic field, and we can test this
Convergent Boundary
Two plates moving towards each other, one plate will be forced under the other, into a subduction zone
Ocean-continent convergent boundary
Ocean is forced under bc more dense, forms OCEANIC TRENCH
melts –> less dense –> rises to continental crust –> continental crust
Ocean-Ocean
Oldest crust forced under, produces volcanic activity
responsible for many oceanic island chains
Continent-Continent
One can be forced under the other, but they do not suduct, does not sink easily
force rocks up into new mountain ranges
if there is some oceanic crust beneath the continental crust, parts of oceanic crust can be moved to mountain tops (scapped up ocean sediment at top of Himalays)
Transform Boundary
Plates slide paste each other
creates transform faults
cause earthquakes
Elastic Rebound theory
plates cannot move continuously, energy and pressure builds up at the fault until it is released all at once in a sudden movement
Supercontinent breakup and life
breakup produces predictable trends in climatic and topographic conditions
- increased biome and species diversity
- increased volcanic activity, global temp.
- shallow seas, sea levels rise
Angle of insolation
angle at which sunlight hits planet
high concentration of solar energy and equator
less energy per surface area at higher or lower latitude
Albedo
reflectivity of a surface
lighter substances have cooling impact
darker substances have a warming impact
Tectonic Plates impact on life and Earth (3)
Snowball Earth bc they were all mainly at equator ~750MA
Global ocean currents transport heat, continents movement can redirect oceanic currents
glaciation + cooling temperature ~50MY
Landform
natural feature of the physical landscape of the Earth
Igneous rock
new rock formed from cooling of molten rock from the mantle, within crust or volcanic eruptions
how all minerals in the crust formed
Metamorphic rock
minerals that have been changed from their original form through intense heat and pressure
takes place under the crust, or at convergent boundaries
Sedimentary rock
rocks formed from the pieces of other rocks or organic material
pressure forces together lowest layers of material into a single structure –>forming a new mineral
Physical Weathering
mechanical break-up of rock,
freeze-thaw cycle
chemical weathering
mineral breakdown by chemical reaction, ex: weak acid
biological weathering
tree roots breaking up rock, parrotfish eating dead corals, lichen using acids to breakdown rocks
Erosion
material which has been weakened though weathering moved from its original location
sometimes very long distances as long as there is energy, when it ends = deposition leads to sedimentation
The rock cycle
igneous is transformed to metamorphic or breaks down to sedimentary
metamorphic break down to
sedimentary
sedimentary can transform into metamorphic