The layer below the crust, with an upper semi-molten part and a lower molten part, containing a deformable region called the asthenosphere
Core
The innermost layer of the Earth, consisting mostly of iron and nickel, divided into an outer molten layer and an inner solid layer
Moho
The boundary between the Earth's crust and mantle, discovered by seismic wave analysis
Continental drift theory
The theory that the continents were once joined in a singlelandmass called Pangaea, which then broke apart and drifted
Seafloor spreading theory
The theory that the mid-ocean ridge is formed by molten rock flowing from a crack in the Earth's crust, pushing the oceanfloorapart as it hardens
Plate tectonics theory
The theory that the Earth's crust is made up of largerigidplates that float on the mantle and move relative to each other, creatingsurfacefeatures like mountains and trenches
7 major tectonic plates
African Plate
Antarctic Plate
Eurasian Plate
Indo-Australian Plate
Pacific Plate
South American Plate
North American Plate
14 minor tectonic plates
Amurian Plate
Arabian Plate
Burma Plate
Caribbean Plate
Caroline Plate
Cocos Plate
Nazca Plate
Okhotsk Plate
Philippine Sea Plate
Scotia Plate
Somali plate
Sunda Plate
Yangtze Plate
New Hebrides Plate
Some tectonic plates are moving towards each other, others are moving apart, and a few are sliding past each other, creating surface features like mountains and trenches
Plates with continents move relatively slowly, about 2 cm per year, while those without continents move faster, about 12 cm per year
Crust
The outermost layer of the Earth
Kinds of crust
Oceanic crust
Continental crust
Mantle
The layer below the crust, with an upper semi-molten part and a lower molten part due to high temperature, containing a deformable region called the asthenosphere
Core
The innermost layer of the Earth, consisting mostly of iron and nickel
Layers of the core
Outer core
Inner core
Outer core
Molten due to intense heat
Inner core
Solid due to extremely high pressure offsetting the melting process from intense heat
Moho
The boundary between the Earth's crust and mantle, discovered by Andrija Mohorovicic through the study of seismic waves
Earthquakes and other explosive activities near the Earth's surface can cause seismic waves
Continental drift theory
Proposed by Alfred Wegener, suggesting that continents were once joined in a single landmass called Pangaea which later broke apart and drifted
Wegener spent the rest of his life searching for evidence to prove his continental drift theory but died in 1930 without convincingly explaining what caused the continents to move
Seafloor spreading theory
Molten rock flowing from a crack in the Earth's crust forms mountains, pushing the ocean floor apart
Plate tectonics theory
Describes the large-scale motion of the Earth's surface, building on continental drift and seafloor spreading concepts
7 major tectonic plates
African Plate
Antarctic Plate
Eurasian Plate
Indo-Australian Plate
Pacific Plate
South American Plate
North American Plate
14 minor tectonic plates
Amurian Plate
Arabian Plate
Burma Plate
Caribbean Plate
Caroline Plate
Cocos Plate
Nazca Plate
Okhotsk Plate
Philippine Sea Plate
Scotia Plate
Somali plate
Sunda Plate
Yangtze Plate
New Hebrides Plate
Some tectonic plates are moving towards each other, others are moving apart, and a few are sliding past each other, creating many of the Earth's surface features like mountains and deep-sea trenches
Plates with continents move relatively slow, about 2 cm per year, while those without continents move faster, about 12 cm per year