older oceanic crust gets destroyed and 'recycled' back into mantle. Newly formed younger crust would not have existed long enough for much sediment to accumulate as it takes place over time. Proves new crust is formed at divergentboundaries at mid ocean ridge, plates move and older crust destroyed
age of rocks supporting TPT
Rocks nearest to crest are youngest and progressively gets older the further it is. Continuous formation pushes older seafloor. Shows that new oceanic crust is created at divergent boundaries, moving laterally on both sides of the mid ocean ridge as seafloor spreading occurs
evidence of magnetic striping
stripes of rock on the seafloor with alternating magnetic properties
magnetic properties
normal polarity
reversed polarity
Normal polarity
earth's magnetic north points to geographical north
earth's magnetic south points to geographical south
Reversed Polarity
earth's magnetic north points to geographical south
earth's magnetic south points to geographical north
geographic north/south
fixed point on earth
magnetic north/south
compass needle points to as it is the earth's magnetic pole
Basalt rocks
forms oceanic crust. it is iron rich and contain magnetic minerals
When basalt erupts from center of mid oceanic ridge
it cools and solidifies, magnetic field of minerals in lava point towards Earth's magnetic north
evidence of magnetic striping supporting TPT
iron-rich lava erupting from centre of ridge cools and solidifies to form new oceanic crust. the crust is pushed in both directions away from centre of the ridge. When earth's polarity reverses, rocksrecord reversals as they have iron-rich minerals. More lava moves away from mid oceanic ridge due to plates diverging, a symmetrical zebra like pattern is formed.
Tectonic plate theory
tectonic plates are constantly moving which result in formation of landforms and phenomena
lithosphere consists of crust and uppermost mantle
mantle is made up of asthenosphere and lower mantle
core is made up of only core
crust is the outermost layer of the earth which is solid and has the lowest temperature. it is the thinnest layer (6-70km).
uppermost mantle and crust make up lithosphere. the are solid and divided into tectonic plates, continental and oceanic
continental
land mass
oceanic
seafloor, denser than continental
asthenosphere is semi solid and the heat from the core causes rocks there to melt