Heat inside Earth and mantle convection

Grade 9 Science Worksheet - Building Confidence

NameDate

Circle the best answer.

  1. Earthquake S waves cannot travel through liquids. S waves from earthquakes do travel through the mantle. Ari reads that plates ride on the mantle. What does card A show about the mantle?

    • The mantle is a liquid, since plates move on it
    • The top of the mantle is solid and the rest is liquid
    • The mantle is solid rock, even though it flows slowly over time
    • The mantle is a gas, since waves pass through it
  2. Hot rock is 3.30 g/cm³. Cooler rock beside it is 3.40 g/cm³. USGS: hotter, lighter material rises. Jun compares two pieces of mantle rock side by side. Using the card, which one moves up, and why?

    • The cooler rock rises because it is denser than the hot rock beside it
    • The hot rock sinks because it holds more heat energy than the cooler rock
    • Neither moves, since both pieces are solid rock held in place
    • The hot rock rises because it is less dense than the cooler rock
  3. Read this first

    Card

    Hot, lighter rock rises; cold, denser rock sinks (USGS). An ocean plate loses heat to the sea for millions of years.

  4. Luz follows an ocean plate that cools for millions of years, then reaches a trench. What does the convection idea predict as it goes down?

    • It rises, because rock near a trench is hotter than the mantle around it
    • It sinks, because cooling made it denser than the hot mantle around it
    • It melts to liquid at once and stops moving, so nothing is carried down
    • It floats, because ocean plates are lighter than the land beside the trench
  5. In heated soup, hot soup rises in the middle, cools at the top and sinks at the sides. USGS compares mantle convection with thick soup heated in a pot. Milo matches the cool soup that sinks at the pot's side. What plays that part in the mantle?

    • Cold slabs sinking at subduction zones
    • The hot core at the bottom of the mantle
    • Plates that stay in one place at the surface
    • Hot rock rising under a mid-ocean ridge
  6. Card (example data)

    Sunlight warms only the top few meters of rock. The mantle starts tens of kilometers down. USGS: Earth's inner heat comes from within.

  7. A student tells Noah that the Sun heats the mantle. Using the card, what is the best reply?

    • No; the mantle has no heat of its own and pressure alone moves the rock
    • Yes; surface heat flows down through the crust until the mantle begins to churn
    • No; sunlight cannot reach it, so the heat comes from decay and leftover heat
    • Yes; the top 100 km of mantle gets Sun heat and passes it down by flowing
  8. Card

    Residual heat is energy left from Earth's formation 4.6 billion years ago. Decay of uranium, thorium and potassium adds heat now (USGS).

  9. Suppose Earth had only residual heat and no decay. What would Pia predict for the mantle's temperature over billions of years?

    • It would cool steadily, with nothing to replace the lost heat
    • It would cool in a single moment and then stay cold
    • It would warm up as old heat is released
    • It would stay the same, since the Sun keeps heating it
  10. Rock is a poor conductor, so heat leaves Earth's interior slowly. Radioactive decay adds heat inside (USGS). Earth formed 4.6 billion years ago, yet Ren notes its interior is still hot. Which explanation fits the card best?

    • Rock cannot lose heat, so the heat stays inside
    • Sunlight reheats the mantle each day, so it cools very little
    • The mantle is a liquid that traps heat and stops it escaping
    • Heat escapes slowly and decay keeps adding more
  11. Card

    Slab pull is a cold, dense slab sinking at a trench and dragging its plate. Ridge push is gravity sliding a plate down from a raised ridge.

  12. Tala studies a plate with a long, cold slab sinking at one edge. Which force fits that edge, using the card?

    • Slab pull, acting at the trench edge
    • Ridge push, since a sinking slab pushes the plate
    • Tidal pull, since the trench is near the coast
    • Ridge push, since the edge is a ridge
  13. Gravity slides a plate away from a raised ridge. A cold, dense slab sinking at a trench drags its plate. Zee draws arrow 1 at a raised ridge pushing a plate away, and arrow 2 at a trench pulling it down. Which labels are correct?

    • Both arrows are slab pull
    • Both arrows are ridge push
    • Arrow 1 is ridge push; arrow 2 is slab pull
    • Arrow 1 is slab pull; arrow 2 is ridge push
  14. Card

    Plates certainly move a few centimeters a year. How many convection cells exist and how they work is still studied (USGS).

  15. Esme sorts statements into known and still studied. Which statement about plate motion is supported by USGS?

    • The exact number of convection cells is known, and so is how each one works
    • Scientists have drilled into the cells to map them directly
    • Whether plates move is still unsettled among scientists
    • Plate motion is certain, but the number and structure of cells are unsettled
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Heat inside Earth and mantle convection

Answer Key - Grade 9 Science Worksheet - Building Confidence

Circle the best answer.

  1. Earthquake S waves cannot travel through liquids. S waves from earthquakes do travel through the mantle. Ari reads that plates ride on the mantle. What does card A show about the mantle?

    • The mantle is a liquid, since plates move on it
    • The top of the mantle is solid and the rest is liquid
    • The mantle is solid rock, even though it flows slowly over time
    • The mantle is a gas, since waves pass through it
  2. Hot rock is 3.30 g/cm³. Cooler rock beside it is 3.40 g/cm³. USGS: hotter, lighter material rises. Jun compares two pieces of mantle rock side by side. Using the card, which one moves up, and why?

    • The cooler rock rises because it is denser than the hot rock beside it
    • The hot rock sinks because it holds more heat energy than the cooler rock
    • Neither moves, since both pieces are solid rock held in place
    • The hot rock rises because it is less dense than the cooler rock
  3. Read this first

    Card

    Hot, lighter rock rises; cold, denser rock sinks (USGS). An ocean plate loses heat to the sea for millions of years.

  4. Luz follows an ocean plate that cools for millions of years, then reaches a trench. What does the convection idea predict as it goes down?

    • It rises, because rock near a trench is hotter than the mantle around it
    • It sinks, because cooling made it denser than the hot mantle around it
    • It melts to liquid at once and stops moving, so nothing is carried down
    • It floats, because ocean plates are lighter than the land beside the trench
  5. In heated soup, hot soup rises in the middle, cools at the top and sinks at the sides. USGS compares mantle convection with thick soup heated in a pot. Milo matches the cool soup that sinks at the pot's side. What plays that part in the mantle?

    • Cold slabs sinking at subduction zones
    • The hot core at the bottom of the mantle
    • Plates that stay in one place at the surface
    • Hot rock rising under a mid-ocean ridge
  6. Card (example data)

    Sunlight warms only the top few meters of rock. The mantle starts tens of kilometers down. USGS: Earth's inner heat comes from within.

  7. A student tells Noah that the Sun heats the mantle. Using the card, what is the best reply?

    • No; the mantle has no heat of its own and pressure alone moves the rock
    • Yes; surface heat flows down through the crust until the mantle begins to churn
    • No; sunlight cannot reach it, so the heat comes from decay and leftover heat
    • Yes; the top 100 km of mantle gets Sun heat and passes it down by flowing
  8. Card

    Residual heat is energy left from Earth's formation 4.6 billion years ago. Decay of uranium, thorium and potassium adds heat now (USGS).

  9. Suppose Earth had only residual heat and no decay. What would Pia predict for the mantle's temperature over billions of years?

    • It would cool steadily, with nothing to replace the lost heat
    • It would cool in a single moment and then stay cold
    • It would warm up as old heat is released
    • It would stay the same, since the Sun keeps heating it
  10. Rock is a poor conductor, so heat leaves Earth's interior slowly. Radioactive decay adds heat inside (USGS). Earth formed 4.6 billion years ago, yet Ren notes its interior is still hot. Which explanation fits the card best?

    • Rock cannot lose heat, so the heat stays inside
    • Sunlight reheats the mantle each day, so it cools very little
    • The mantle is a liquid that traps heat and stops it escaping
    • Heat escapes slowly and decay keeps adding more
  11. Card

    Slab pull is a cold, dense slab sinking at a trench and dragging its plate. Ridge push is gravity sliding a plate down from a raised ridge.

  12. Tala studies a plate with a long, cold slab sinking at one edge. Which force fits that edge, using the card?

    • Slab pull, acting at the trench edge
    • Ridge push, since a sinking slab pushes the plate
    • Tidal pull, since the trench is near the coast
    • Ridge push, since the edge is a ridge
  13. Gravity slides a plate away from a raised ridge. A cold, dense slab sinking at a trench drags its plate. Zee draws arrow 1 at a raised ridge pushing a plate away, and arrow 2 at a trench pulling it down. Which labels are correct?

    • Both arrows are slab pull
    • Both arrows are ridge push
    • Arrow 1 is ridge push; arrow 2 is slab pull
    • Arrow 1 is slab pull; arrow 2 is ridge push
  14. Card

    Plates certainly move a few centimeters a year. How many convection cells exist and how they work is still studied (USGS).

  15. Esme sorts statements into known and still studied. Which statement about plate motion is supported by USGS?

    • The exact number of convection cells is known, and so is how each one works
    • Scientists have drilled into the cells to map them directly
    • Whether plates move is still unsettled among scientists
    • Plate motion is certain, but the number and structure of cells are unsettled