Key Terms - Plate Tectonics Flashcards
Core (4)
Densest, hottest part of the planet
Made of rocks rich in iron and nickel
Temps can exceed 5000ยฐC
Heat is from primordial and radiogenic heat
Primordial heat
Heat left from the earths formation
Radiogenic heat
Heat produced by the radioactive decay of isotopes
Mantle (3)
Surrounds the core
Thickest layer made of silica rocks rich in iron and magnesium
Upper mantles is semi molten and is known as aesthenosphere
Crust (2)
Thinnest outer solid layer
Tow types of crust = oceanic and continental
Oceanic crust (3)
Found beneath the world oceans
Composed of relatively dense basalt
Between 6-10km thick
Formed at spreading mid oceans ridges at constructive margins
Continental crust (5)
Forms the continents
Thicker and older
Can be up to 70km thick
Composed of granite
Formed at subduction zones
Lithosphere
The crust and rigid upper mantle
Aesthenosphere (2)
The semi-molten upper mantle
Below the lithosphere
Plate tectonic theory (2/5)
Suggests the crust is divided into tectonic plates that move due to convection in the aesthenosphere
Movement = mid-ocean ridges, ocean trenches, fold mountains and causes earthquakes and volcanoes
Alfred Wegener (3)
Published a theory in 1912 suggesting there was once a super continent caused Pangea and that overtime the landmasses drifted apart
Theory based on evidence = geological, climatological, biological
He counsels exp,Ian how the continent ps moved though
Mid - Atlantic ridge (3)
Continuous uplift feature that runs down the centre of the Atlantic Ocean
The central part of the ridge is marked by a Central Valley
First seen in 1940s when the ocean floor was first mapped
Sea floor spreading (5)
Surveys of the ocean floor established
Rocks found closest to mid oceanic ridges = youngest
Rocks nearest the Continental landmasses were the oldest
Supports idea that sea floors are spreading out from mid oceanic ridges where new crust was being formed
Magma reached the surface as two oceanic plates moved apart at a constructive margin
Palaeomagnetism (5)
Rocks that form the ocean floor show stripes of alternating polarity
Lavas that erupt at mid-oceanic ridges contain iron which aligns to the Earthโs polarity = fixed when the lava solidifies.
Earthโs magnetic field reverses 4 to 5 times per million years.
These switches are recorded in the rocks of the ocean floor as a series of โmagnetic stripesโ with rocks aligned alternatively towards north and south poles.
The pattern suggests that ocean crust is spreading out from the mid- ocean boundary
Convection currents (3)
High temps at Earthโs core help create continuous convection currents in the aesthenosphere that transfer heat from the core to the Earthโs surface.
As the heated magma spreads out underneath the crustal plates it causes them to move due to traction.
The magma then cools, becomes denser and sinks downwards again.