S6E5a. Compare and contrast the Earth's crust, mantle, and core including temperature, density, and composition.
Name the 4 main layers of the Earth
Crust
Mantle
Outer Core
Inner Core
Basic Layers Percent of Earth's mass
Crust
Mantle
Core
Crust
Thinnest layer of the Earth, part of the lithosphere
Crust
Made up of large amounts of SILICON AND ALUMINUM
Composed of plates on which the continents and oceans rest. These "ride" over molten mantle
Crust is part of the lithosphere
Two types of Crust: Oceanic and Continental
Continental vs. Oceanic Crust
Continental
Oceanic
Continental Crust
Rock Type: Granite
Thickness: 5 – 70km (Thicker)
State: Solid
Crust Age: 4 billion years old or Older
Density: Less Dense
Element Composition: Oxygen, Sodium, Silicon, Aluminum, Potassium
Oceanic Crust
Rock Type: Basalt
Thickness: 3 – 8 km (Thinner)
State: Solid
Crust Age: 180 million years old or Younger
Density: More Dense
Element Composition: Iron, Magnesium, Calcium
Lithosphere
The crust and the upper layer of the mantle together make up a zone of rigid, brittle rock called the Lithosphere.
Lithosphere
The lithosphere (crust and upper mantle) is divided into separate plates which move very slowly in response to the "convection" part of the mantle.
Lithospheric Plates
The crust of the Earth is broken into many pieces called plates. The plates "float" on the soft, semi-rigid asthenosphere.
Mantle
Upper Mantle
Lower Mantle
Middle Mantle
Mantle
The Mantle is the largest layer of the Earth at 2900 km thick. The middle mantle is composed of very hot dense rock that flows like asphalt under a heavy weight. The movement of the middle mantle (asthenosphere) is the reason that the crustal plates of the Earth move.
Asthenosphere
The asthenosphere is the semi-rigid part of the middle mantle that flows like hot asphalt under a heavy weight.
Convection Currents
The middle mantle "flows" because of convection currents. Convection currents are caused by the very hot material at the deepest part of the mantle rising being less dense, then cooling becoming more dense and sinking again --repeating this cycle over and over.
Mantle
Solid but capable of flow (like fudge)
Semi-Solid/Semi Liquid
Thickest layer of the Earth 2900km (1800 miles)
Element Composition: Magnesium, Silicon, Oxygen, and Iron
The hot magma rises then cools and sinks
These convection currents cause changes in the Earth's surface
Conveyor belt for the tectonic plates
Mantle
Upper Mantle
Convection Currents
Middle Mantle
Lower Mantle
Core
Inner Core
Outer Core
Outer Core
Composition: Molten (liquid) metal that is about 4,700°C (8,500°F)
Thickness: 2,266 km (1,400) miles
State of Matter: Composed of the melted metals nickel and iron (liquid)
Located about 1,800 miles beneath the crust.
Inner Core
Solid sphere made mostly of iron and has Nickel
It is believed to be as hot as 6,650°C (12,000°F)
Heat in the core generated by the radioactive decay of uranium and other elements
It is solid because of the pressure from the outer core, mantle, and crust compressing it.
Thickness: 1271 km (800 miles)
Temperature increases as depth increases
Depth
Density and Pressure increase as depth increases
Scientists have drilled 7.6 miles into the earth, which is only 0.2% of the distance to the earth's core
How do we know so much about what's under Earth's surface?
Through INDIRECT EVIDENCE, mostly from seismic waves caused by earthquakes. Sometimes indirect evidence is the only option for scientists to develop a theory
Big Ideas
The Earth is divided into 3 Main Layers: Crust, Mantle, Core
Main Rock type of the 2 types of Crust: Oceanic - Basalt, Continental - Granite
Oceanic Crust is denser than Continental Crust
The lithosphere is divided into tectonic plates
The Mantle has the convection currents which causes the plates to move
The Asthenosphere flows semi-liquid on which the plates move
Temperature, pressure, and density increases as depth increases. This is a direct relationship.