The Earth and its layers

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GLGY 209-UofC

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25 Terms

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How deep is the earth?

6,4000 km deep

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What is drilling?

  • way for scientists to probe the Earth's sediments, crust, and upper mantle

  • Deepest drill hole– 12 km 

  • Marianas trench max 11km- is what we know 

  • We have to learn about the interior of the earth through other observation 

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What is the different criteria used to discuss earth’s internal layers?

  • Chemical composition 

  • Mechanical behavior of materials 

    • When a force is applied=how they respond

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How many many layers is the earth composed of?

  • 3

  • Outer: crust, Mantle, Innermost: Core (boiled egg)

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How do we know the layers are there?

  • Measured through seismic waves which are measured at stations across the earth

  • the speed of these waves increases with density and as you go deeper into the earth the density of rocks increases due to presuure from overlying rocks

  • Major change in seismic wave velocities=the density is significantly changing–seismic discontinuity

    • These changes say there are different layers 

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What are the differnet kinds of earthquake waves?

  • P-wave (body wave), S-wave (surface/shear waves)

    • P-waves travel through compression and decompression

    • P-waves are faster 

  • P-waves can travel through solids (rocks and minerals) and fluids (water and magma). S-waves can only travel through solids.  

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How are these waves read?

  • Seismic station is where a sensor is 

    • P-wave arrives first and then the s- wave arrives later 

  • Speed is determined on the function of the property of the rock  

    • Less dense=slower dense=faster 

    • Affects both waves 

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What is the crust?

  • thick outer shell of rock, referring to less than (<) 1% of the planets radius and volume

  • 2 types: continental and oceanic

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What is continental crust?

  • Thicker—Avg–25-30 km, but avg can vary (Himalayas-thick crust (80km)) 

  •  30% of crust and high elevation

  • avg composed of granite (density 2.6-2.7g/cm relative to water)

  • Continents are formed at higher elevations because basalt/oceanic crust is floating on the earth's mantle, continental crust floats higher (forms ocean basisn)

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What is oceanic crust?

  • Thinner—Avg 5-7km—Fairly uniform in thickness 

  • 70% of the crust and low elevation

  • made of basalt (density: 2.9-3g/cm relative to water)

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What is a hypsometric curve?

  • shows the proportion of the earth's surface at a certain elevation 

    • Distribution of land surface relative to sea level 

    • Continental shelf: edge of a continent that lies under the ocean (submerged)

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What is the mantle?

  • Largest and thickest layer 

  • 82% of Earth by volume 

  • Generally solid rock despite magma, but can behave like a fluid sometimes (over long tome scales, the rock can move) 

  • Seismic wave activity increases

    • Show a sharp increase in speed from the base of the crust to the top of the mantle 

  • Divisible into 

    • Upper mantle (base to 410 km depth)

    • Transitional mantle (mineralogical changes) 

    • Lower mantle (660-2,900km) 

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What is the upper mantle composed of?

  • ultramafic rock peridotite

    • Peridotite–most common mantle rock 

      • Basalt is volcanic, magma is formed in mantle, and as its moved up it carries fragments of the mantle (Xenolith)

      • Xeno=foreign Lith=Rock, foreign rock 

    • Ultramafic–extremely rich in iron and magnesium (even more dense)

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Why is the mantle similar to a pot of water heated from below?

  • Below certain depth, mantle convects

  • Convection currents occur due to density differences caused by variations in temperature and composition

  • As it heats up, the bottom gets hotter and moves up and cold comes down—Convection cell 

  • Over long time scales, the mantle can slowly move/flow 

  • Over short time scales it behaves as a solid 

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What is the core?

  • 17% of Earth by volume 

    • Base of mantle to center

  • composed of outer and inner core

  • Core has a composition similar to iron meteorite 

    • Shooting stars that reach earth and they have a crust, mantle and core 

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What is the outer core?

  • Liquid iron and nickel 

  • Know because of seismic waves 

  • P-wave speed decreases, and s-waves don't travel through 

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What is the inner core?

  • Solid 

  • Primarily composed of iron and nickel 

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How is earths magnetic field produced?

  • Outer core flows around the solid inner core generates earth's magnetic field (the motion creates the magnetic field)

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What does the magnetic field do?

  • shields us from high energy radiation from the sun

    • Also use for navigation 

    •  Interacts with solar waves and protects us 

    • Interaction between high energy particles and magnetic field creates aurora

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What are compositional layers?

  • continental and oceanic crust, mantle and core 

  • Behavior of the layers is different how they respond to force 

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What are the mechanical layers?

The lithosphere, the asthenosphere, the mesosphere, the outer core, and the inner core

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How do the layers act?

  • The crust and a bit of the upper mantle behave in a rigid way (break rather than flow)

  • lithosphere doesn’t take part in convection

  • Asthenosphere–convects 

  • Lower mantle is also rigid-pressure is too high–Mesosphere

  • Outer core convects, inner is solid rock so doesn't convect because of high pressures  

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What is the lithosphere?

  • the outermost physical layer of the earth (crust and upper part of mantle)

    • Diamonds form because its thick and there's high pressure 

  • 2 types: oceanic and continental

  • It is broken into segments called plates

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What is the asthenosphere?

  • from the base of the lithosphere to the transitional mantle

  • moves and flows due to convection currents created by heat coming from the earth’s core

  • is relatively unbroken (determined this by analyzing seismic waves that pass through the layers)

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What is the mesosphere?

  • the lower mantle, is more rigid due to high pressures and temperatures

  • Located at a depth of approximately 410 and 660 km below the earth’s surface

  • extreme conditions create a transition zone in the upper mesosphere where minerals continuously change