The structure of the Earth consists of various spherical shells or layers that can be categorized in two manners:
a) Chemical/ Elemental compositions
b) Mechanical/physical properties
more commonly discussed layers of earth; layers are defined based on its chemical or elemental composition
COMPOSITIONAL (CHEMICAL) LAYERS OF EARTH
LAYERS OF EARTH
CRUST
MANTLE
CORE
Consist of several elements
CRUST
3 to 5 miles thick under the ocean and approximately 25 miles thick under the continents
CRUST
ELEMENTS IN THE CRUST
46.6 OXYGEN
27.7 SILICON
TYPRES OF CRUST
OCEANIC CRUST (Basaltic) 71%
CONTINENTAL CRUST (Granitic) 29%
Sediments coat the seafloor, thickest near the shore
OCEANIC CRUST (Basaltic) 71%
Composed of magma that erupts on the seafloor to create basalt lava flow; or cools deeper down to create igneous rock gabbro
OCEANIC CRUST (Basaltic) 71%
Made up of different types of rocks
CONTINENTAL CRUST (Granitic) 29%
Average composition is granite which is less dense than mafic igneous rocks oceanic crust
CONTINENTAL CRUST (Granitic) 29%
Thicker part of the crust
CONTINENTAL CRUST (Granitic) 29%
Layer under the crust, compromises 82% of Earth volume
MANTLE
About 1, 800 miles deep
MANTLE
About 1, 800 miles deep
MANTLE
Heat causes rocks to rise
MANTLE
TYPES OF MANTLE
CONVECTION
CONDUCTIO
heat transfer through rapid collision of atoms which only happens in solid
CONDUCTION
heat flows from warmer to cooler places until it reaches same temperature
CONDUCTION
process of material that can move and flow and develops convection currents
CONVECTION
Center of the Earth made of 85% iron metal and 15% nickel
CORE
TYPES OF CORE
INNER CORE
OUTER CORE
Solid part of the core made of iron
Inner core
Has a radius of about 760 miles according to NASA
Inner core