tectonicplates - called lithospheric plate is a massive, irregularly shaped slab of solid rock composed of both continentsl and oceanic lithosphere
3 changes in earth surface
continental drift theory
Seafloor spreading
Theory of plate tectonics
Continentsl drif theory - the continents drifted apart and collided to form the supercontinent Pangea
continental drift theory was proposed by Alfred Wegener in 1912
continental drift theory- the break up of the supercontinent
Sea floor spreading - The movement of oceanic crust away from the mid-ocean ridge
Sea floor spreading is the process where two tectonic plates move away from each othe then the rock breaks and forms a crack between the plates
Plate Tectonics - The theory that Earth's outer layer is made up of several large pieces called plates
Continental drift - The theory that the continents are slowly moving apart or coming together
Mid-Ocean Ridge - A chain of mountains under the sea which runs through the Atlantic Ocean
Continental drift - A hypothesis proposed by Alfred Wegener to explain how continents could have moved apart over time.
Sea floor spreading was formulated by a geologist and nary submarine commandar Harry Hess
Theory of plates tectonics - the solid part of earth composed of seven major subjects and several minor parts called plates
Compositional layers
A) Crust
B) Mantle
C) Core
Mechanical layers
A) Lithosphere
B) Asthenosphere
C) Mesosphere
D) outher core
E) Inner core
howdidthescientistbelievewegener - they discovered that magma is rising up through cracks ( how new lands is created )
howdidthescientistbelievewegener - they have been plotting the locations of earthquakes and volcanos and observes that follow the pattern that wegener explained
Theplatestectonics theory is based on concepts proposed by Alfred wegener
Thelithosphere is divided into continent-sized plates that are constantly moving
Thecontinents were once part of the supercontinents called pangaea
lithosphereplates moves 1-2 inches a year
boundaries are where plates meet
3types of plate tectonic
conceraent - where plate meets/collides
Transform - where plate slides past one another
divergent- where plates move apart
Volcanoesandmountains form as a result of convergent boundaries colliding
Earthquakes and tsunamis accur at convergent and transformboundaries
fissures, cracksandrifts in the surface occurs at divergent boundaries
Seafloorspreading occurs at divergent boundaries on the ocean floor
TRANSFORM PLATE BOUNDARY - Plates slide against each other in opposite directions. No mountains or volcanoes are formed but only earthquake results. No subduction, no volcanoes and magma
crust is the outer layer of the Earth
the mantle is made up of magma and rock
Plate tectonics is the theory that explains how the continents move around the world.
lithosphere is broken into many small and large slabs of rocks called tectonic plates
The process by which the ocean floor sinks beneath a deep-ocean trench and back into the Mantle is called subduction
The place where two plates move apart is called a divergentboundaries
a oceanridge is a long chain of mountains that is found underwater
the process continuously adds new material To The ocean floor is called seafloorspreading
A deepoceantrench is a deep underwater canyon
A place where two plates slip past each other is called a transform boundaries
a well-tested concept that explains the wild range of a wide range of observations is called a scientific theory
The place where two plates come together is called a divergent boundaries