Features of the ocean floor

Grade 9 Science Worksheet - Challenge Me

NameDate

Circle the best answer.

  1. Read this first

    Card (example)

    Sea floor 500 km from a ridge crest is 20 million years old. Magma rises at the crest and hardens into new floor. Old floor sinks at trenches. Some continental rock is billions of years old.

  2. A student tells Esme the sea floor is as old as the continents. Which reply is best supported by the card?

    • Yes; magma rising at ridges keeps adding new floor and no floor is lost anywhere
    • No; floor is made at ridges and recycled at trenches, so it is much younger
    • Yes; both formed together when Earth cooled, and neither has changed since then
    • No; the sea floor is older, since it lies below the continents and formed first
  3. Card

    Trenches are narrow and 8 to 10 km deep (USGS). They lie beside curved chains of volcanoes. Deep ocean currents move slowly (example).

  4. A student tells Jun that deep currents carved the trenches. Which reply is best supported by the card?

    • No; currents cannot cut a trench 8 to 10 km deep beside volcanoes; plate convergence fits
    • Yes; deep currents carve trenches the same way rivers cut canyons on land, but deeper
    • No; trenches form where plates part, and volcanoes then fill the trenches with rock
    • Yes; the volcanoes beside trenches are built from the rock that currents eroded
  5. Card (NOAA)

    The mid-ocean ridge spans 40,389 miles, about 90% under the ocean. 1 mile is 1.609 km. Example, rounded: the Andes, the longest range on land, stretch about 7,000 km.

  6. A student tells Kira that ridges are small next to land mountain ranges. Which reply fits the card?

    • Yes; at about 6,500 km the ridge is shorter than the Andes, so it is small by comparison
    • Yes; just the part above water counts as a mountain range, so the ridge is small
    • No; at about 65,000 km the ridge is many times the Andes, but about 90% is underwater
    • No; the ridge is about 65,000 km long, though it lies entirely above the water line
  7. Card (example data)

    a submersible descends at 0.5 m per second, explores for 1 hour, then rises at 1 m per second. The average ocean depth is 3,682 m (NOAA).

  8. Luz plans a dive to the average ocean depth. About how long is the whole trip?

    • About 4.1 hours
    • About 5.1 hours
    • About 2.0 hours
    • About 3.1 hours
  9. Card (example, rounded)

    Water pressure rises 1 atmosphere (atm) for every 10 m of depth, on top of 1 atm at the surface. NOAA: average depth 3,682 m; deepest about 10,935 m.

  10. How much more pressure is there at the deepest point than at the average depth, by Milo's math?

    • About 725 atm more
    • About 1,094 atm more
    • About 7,253 atm more
    • About 72 atm more
  11. Card (approximate model, example)

    Sea-floor depth in meters is about 2,500 + 350 × √(age in millions of years). Young floor near a ridge is hot and shallow; it deepens as it cools.

  12. Floor spreads from a ridge at 4 cm a year. How far from the ridge is floor that is 5,300 m deep, by Noah's math? (1 km = 100,000 cm.)

    • About 320 km
    • About 2,560 km
    • About 256 km
    • About 25,600 km
  13. Card (example data)

    a ridge flank deepens 1,400 m over 700 km. The unknown belt beside curved volcanic islands deepens from 4,000 m to 10,000 m over 60 km.

  14. Which feature is the belt, and why, by Ren's reading?

    • A continental slope, since it drops steeply beside the volcanic islands
    • A trench: it drops about 50 times more steeply than a ridge flank
    • A trench: it drops about 5 times more steeply than a ridge flank
    • A ridge flank, since depth changes with distance along both of them
  15. Claim: new sea floor forms at a ridge crest and spreads away on both sides. Which evidence would most strengthen the claim, by Tala's reading?

    • A photo of fresh black rock at the crest taken by a submersible, showing new lava
    • The crest's height compared with the heights of other mountain ranges on land
    • Dated rock samples showing that ages rise with distance from the crest on both sides
    • Depth readings along one line that deepen away from the crest on both of its sides
  16. The average ocean depth is about 3,682 m. The deepest point is about 10,935 m. Which statement does the card support, by Ari's math?

    • The deepest point is about one-third of the average depth and about 7,250 m deeper
    • The deepest point is about 3 times the average depth and about 7,250 m deeper
    • The deepest point is about 3 times the average depth and about 14,600 m deeper
    • The deepest point is about 30 times the average depth and about 7,250 m deeper
  17. Card (NOAA)

    Ridges form where plates push apart and magma rises; trenches form where plates converge and one moves under the other; seamounts are volcanic mountains. Sediment settles on abyssal plains.

  18. Which summary links each feature to how it forms, by Bo's reading?

    • Ridges: plates part. Trenches: wave erosion cuts them. Seamounts: volcanoes. Plains: settled sediment
    • Ridges: plates part. Trenches: plates meet, one sinks. Seamounts: volcanoes. Plains: settled sediment
    • Ridges: plates meet and one sinks. Trenches: plates part. Seamounts: volcanoes. Plains: settled sediment
    • Ridges: plates part. Trenches: plates meet, one sinks. Seamounts: settled sediment. Plains: volcanoes
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Features of the ocean floor

Answer Key - Grade 9 Science Worksheet - Challenge Me

Circle the best answer.

  1. Read this first

    Card (example)

    Sea floor 500 km from a ridge crest is 20 million years old. Magma rises at the crest and hardens into new floor. Old floor sinks at trenches. Some continental rock is billions of years old.

  2. A student tells Esme the sea floor is as old as the continents. Which reply is best supported by the card?

    • Yes; magma rising at ridges keeps adding new floor and no floor is lost anywhere
    • No; floor is made at ridges and recycled at trenches, so it is much younger
    • Yes; both formed together when Earth cooled, and neither has changed since then
    • No; the sea floor is older, since it lies below the continents and formed first
  3. Card

    Trenches are narrow and 8 to 10 km deep (USGS). They lie beside curved chains of volcanoes. Deep ocean currents move slowly (example).

  4. A student tells Jun that deep currents carved the trenches. Which reply is best supported by the card?

    • No; currents cannot cut a trench 8 to 10 km deep beside volcanoes; plate convergence fits
    • Yes; deep currents carve trenches the same way rivers cut canyons on land, but deeper
    • No; trenches form where plates part, and volcanoes then fill the trenches with rock
    • Yes; the volcanoes beside trenches are built from the rock that currents eroded
  5. Card (NOAA)

    The mid-ocean ridge spans 40,389 miles, about 90% under the ocean. 1 mile is 1.609 km. Example, rounded: the Andes, the longest range on land, stretch about 7,000 km.

  6. A student tells Kira that ridges are small next to land mountain ranges. Which reply fits the card?

    • Yes; at about 6,500 km the ridge is shorter than the Andes, so it is small by comparison
    • Yes; just the part above water counts as a mountain range, so the ridge is small
    • No; at about 65,000 km the ridge is many times the Andes, but about 90% is underwater
    • No; the ridge is about 65,000 km long, though it lies entirely above the water line
  7. Card (example data)

    a submersible descends at 0.5 m per second, explores for 1 hour, then rises at 1 m per second. The average ocean depth is 3,682 m (NOAA).

  8. Luz plans a dive to the average ocean depth. About how long is the whole trip?

    • About 4.1 hours
    • About 5.1 hours
    • About 2.0 hours
    • About 3.1 hours
  9. Card (example, rounded)

    Water pressure rises 1 atmosphere (atm) for every 10 m of depth, on top of 1 atm at the surface. NOAA: average depth 3,682 m; deepest about 10,935 m.

  10. How much more pressure is there at the deepest point than at the average depth, by Milo's math?

    • About 725 atm more
    • About 1,094 atm more
    • About 7,253 atm more
    • About 72 atm more
  11. Card (approximate model, example)

    Sea-floor depth in meters is about 2,500 + 350 × √(age in millions of years). Young floor near a ridge is hot and shallow; it deepens as it cools.

  12. Floor spreads from a ridge at 4 cm a year. How far from the ridge is floor that is 5,300 m deep, by Noah's math? (1 km = 100,000 cm.)

    • About 320 km
    • About 2,560 km
    • About 256 km
    • About 25,600 km
  13. Card (example data)

    a ridge flank deepens 1,400 m over 700 km. The unknown belt beside curved volcanic islands deepens from 4,000 m to 10,000 m over 60 km.

  14. Which feature is the belt, and why, by Ren's reading?

    • A continental slope, since it drops steeply beside the volcanic islands
    • A trench: it drops about 50 times more steeply than a ridge flank
    • A trench: it drops about 5 times more steeply than a ridge flank
    • A ridge flank, since depth changes with distance along both of them
  15. Claim: new sea floor forms at a ridge crest and spreads away on both sides. Which evidence would most strengthen the claim, by Tala's reading?

    • A photo of fresh black rock at the crest taken by a submersible, showing new lava
    • The crest's height compared with the heights of other mountain ranges on land
    • Dated rock samples showing that ages rise with distance from the crest on both sides
    • Depth readings along one line that deepen away from the crest on both of its sides
  16. The average ocean depth is about 3,682 m. The deepest point is about 10,935 m. Which statement does the card support, by Ari's math?

    • The deepest point is about one-third of the average depth and about 7,250 m deeper
    • The deepest point is about 3 times the average depth and about 7,250 m deeper
    • The deepest point is about 3 times the average depth and about 14,600 m deeper
    • The deepest point is about 30 times the average depth and about 7,250 m deeper
  17. Card (NOAA)

    Ridges form where plates push apart and magma rises; trenches form where plates converge and one moves under the other; seamounts are volcanic mountains. Sediment settles on abyssal plains.

  18. Which summary links each feature to how it forms, by Bo's reading?

    • Ridges: plates part. Trenches: wave erosion cuts them. Seamounts: volcanoes. Plains: settled sediment
    • Ridges: plates part. Trenches: plates meet, one sinks. Seamounts: volcanoes. Plains: settled sediment
    • Ridges: plates meet and one sinks. Trenches: plates part. Seamounts: volcanoes. Plains: settled sediment
    • Ridges: plates part. Trenches: plates meet, one sinks. Seamounts: settled sediment. Plains: volcanoes