Forces that build land up and wear it down

Grade 9 Science Worksheet - Challenge Me

NameDate

Circle the best answer.

  1. Read this first

    Model card (example data)

    Crust 2.7 g/cm³ floats on mantle 3.3 g/cm³. As rock is removed, the crust floats up by 2.7/3.3 of the thickness removed.

  2. A student says removing 3,300 m of rock lowers a range's peaks by 3,300 m. Milo uses the model card. What is the net lowering?

    • About 3,300 m, since peaks drop by the thickness eroded
    • The peaks rise 2,700 m, since erosion lifts the crust
    • About 600 m, since the crust rebounds about 2,700 m as the load is removed
    • About 2,700 m, since the rebound is the lowering
  3. A student says a range rising 1 cm a year (USGS) will be 100 km taller in 10 million years. Luz checks the claim. What is its main flaw?

    • Mountains cannot rise, since weathering wins over uplift in the long run
    • It ignores erosion and changing rates over millions of years
    • Uplift slows when erosion piles sediment on the peaks
    • The rate is too small: 1 cm a year adds just 10 km in 10 million years, not 100 km
  4. A, 0.04, 0.04, 60 cm, steady; B, 0.04, 0.25, bare rock; C, 0.04, 0.01, 120 cm, thickening. A student claims weathering and erosion always run at the same rate. Jun checks the table. Which reply fits?

    • Yes: sites A and C both hold soil, so their rates must be equal
    • No: weathering moves soil away at sites B and C, which leaves rock bare
    • Yes: soil is made at 0.04 mm a year everywhere, so erosion must match it
    • No: they match only at site A; site B is bare and site C is deepening
  5. Model card (example data)

    Crust 2.7 g/cm³ floats on mantle 3.3 g/cm³. As rock is removed, the crust floats up by 2.7/3.3 of the thickness removed.

  6. Erosion removes 20 m of rock per million years from a range. Bo uses the model card. How long to lower its peaks by 600 m?

    • About 30 million years
    • About 165 million years
    • About 37 million years
    • About 1.65 million years
  7. Sea-floor limestone now lies 2,700 m up. Noah weighs two explanations: the land rose, or the sea once stood that high. Which evidence would best decide?

    • A date showing the limestone formed on the sea floor
    • The same marine layer lies at sea level on a coast 300 km away
    • More marine fossils found in the plateau rock, of many kinds and ages
    • Limestone layers that lie flat
  8. A catchment was logged in 2015. Ren designs a test of whether erosion there has increased. Which measurement is most informative?

    • Soil depth measured at one hilltop after logging
    • Sediment past a gauge before and after, in years with matching rainfall
    • Sediment carried past the gauge after logging, measured in one very wet year
    • Rainfall totals measured before and after logging
  9. A study measures 0.2 mm a year of erosion at one rock outcrop. A writer claims the whole range erodes at that rate. Tala grades the claim. What is the best verdict?

    • Strongly supported: a measured rate applies everywhere in a range
    • Not supported: erosion rates cannot be measured
    • Weakly supported: one outcrop cannot represent a varied range
    • Supported: a precise measurement at one place is precise everywhere
  10. Three sites (example data)

    SiteUplift (mm/yr)Erosion (mm/yr)Height trend
    P55steady
    Q01falling
    R62rising
  11. Zee reads the table. Which summary of what sets height fits all three sites?

    • Height follows erosion alone, so R at 2 mm a year is the lowest site
    • Height follows uplift alone, so P at 5 mm a year must be rising
    • Height follows uplift minus erosion: steady at P, falling at Q, rising at R
    • Height follows whichever rate is larger, so P is falling
  12. Table, Three climates (example data), with columns Site, Mean temperature (°C), Rain (mm/yr), Weathering seen

    Alpine, -2, 900, frost-split blocks, little clay; Rainforest, 25, 3,000, deep clay soil, few fragments; Desert, 22, 100, thin rock crumbs, little clay.

  13. Esme reads the table. Which summary of weathering fits all three sites?

    • Cold sites favor physical breakup; warm, wet sites favor chemical change
    • Warmth alone drives chemical weathering, since the 22 °C desert made clay
    • The three sites show chemical weathering at the same rate
    • Wet sites break rock into blocks, while cold sites turn it to clay
  14. Ari runs uplift of 0.5 mm a year against erosion of 0.4 mm a year for 10 million years (example data). Which summary fits?

    • Net gain is 9,000 m, since both processes move rock
    • Net gain is 1,000 m, the gap between 5,000 m and 4,000 m, so a 10% error in erosion shifts it by 400 m
    • Net gain is 1,000 m, and a small rate error cannot change it much
    • Net gain is 5,000 m, the larger total, whatever the erosion rate
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Forces that build land up and wear it down

Answer Key - Grade 9 Science Worksheet - Challenge Me

Circle the best answer.

  1. Read this first

    Model card (example data)

    Crust 2.7 g/cm³ floats on mantle 3.3 g/cm³. As rock is removed, the crust floats up by 2.7/3.3 of the thickness removed.

  2. A student says removing 3,300 m of rock lowers a range's peaks by 3,300 m. Milo uses the model card. What is the net lowering?

    • About 3,300 m, since peaks drop by the thickness eroded
    • The peaks rise 2,700 m, since erosion lifts the crust
    • About 600 m, since the crust rebounds about 2,700 m as the load is removed
    • About 2,700 m, since the rebound is the lowering
  3. A student says a range rising 1 cm a year (USGS) will be 100 km taller in 10 million years. Luz checks the claim. What is its main flaw?

    • Mountains cannot rise, since weathering wins over uplift in the long run
    • It ignores erosion and changing rates over millions of years
    • Uplift slows when erosion piles sediment on the peaks
    • The rate is too small: 1 cm a year adds just 10 km in 10 million years, not 100 km
  4. A, 0.04, 0.04, 60 cm, steady; B, 0.04, 0.25, bare rock; C, 0.04, 0.01, 120 cm, thickening. A student claims weathering and erosion always run at the same rate. Jun checks the table. Which reply fits?

    • Yes: sites A and C both hold soil, so their rates must be equal
    • No: weathering moves soil away at sites B and C, which leaves rock bare
    • Yes: soil is made at 0.04 mm a year everywhere, so erosion must match it
    • No: they match only at site A; site B is bare and site C is deepening
  5. Model card (example data)

    Crust 2.7 g/cm³ floats on mantle 3.3 g/cm³. As rock is removed, the crust floats up by 2.7/3.3 of the thickness removed.

  6. Erosion removes 20 m of rock per million years from a range. Bo uses the model card. How long to lower its peaks by 600 m?

    • About 30 million years
    • About 165 million years
    • About 37 million years
    • About 1.65 million years
  7. Sea-floor limestone now lies 2,700 m up. Noah weighs two explanations: the land rose, or the sea once stood that high. Which evidence would best decide?

    • A date showing the limestone formed on the sea floor
    • The same marine layer lies at sea level on a coast 300 km away
    • More marine fossils found in the plateau rock, of many kinds and ages
    • Limestone layers that lie flat
  8. A catchment was logged in 2015. Ren designs a test of whether erosion there has increased. Which measurement is most informative?

    • Soil depth measured at one hilltop after logging
    • Sediment past a gauge before and after, in years with matching rainfall
    • Sediment carried past the gauge after logging, measured in one very wet year
    • Rainfall totals measured before and after logging
  9. A study measures 0.2 mm a year of erosion at one rock outcrop. A writer claims the whole range erodes at that rate. Tala grades the claim. What is the best verdict?

    • Strongly supported: a measured rate applies everywhere in a range
    • Not supported: erosion rates cannot be measured
    • Weakly supported: one outcrop cannot represent a varied range
    • Supported: a precise measurement at one place is precise everywhere
  10. Three sites (example data)

    SiteUplift (mm/yr)Erosion (mm/yr)Height trend
    P55steady
    Q01falling
    R62rising
  11. Zee reads the table. Which summary of what sets height fits all three sites?

    • Height follows erosion alone, so R at 2 mm a year is the lowest site
    • Height follows uplift alone, so P at 5 mm a year must be rising
    • Height follows uplift minus erosion: steady at P, falling at Q, rising at R
    • Height follows whichever rate is larger, so P is falling
  12. Table, Three climates (example data), with columns Site, Mean temperature (°C), Rain (mm/yr), Weathering seen

    Alpine, -2, 900, frost-split blocks, little clay; Rainforest, 25, 3,000, deep clay soil, few fragments; Desert, 22, 100, thin rock crumbs, little clay.

  13. Esme reads the table. Which summary of weathering fits all three sites?

    • Cold sites favor physical breakup; warm, wet sites favor chemical change
    • Warmth alone drives chemical weathering, since the 22 °C desert made clay
    • The three sites show chemical weathering at the same rate
    • Wet sites break rock into blocks, while cold sites turn it to clay
  14. Ari runs uplift of 0.5 mm a year against erosion of 0.4 mm a year for 10 million years (example data). Which summary fits?

    • Net gain is 9,000 m, since both processes move rock
    • Net gain is 1,000 m, the gap between 5,000 m and 4,000 m, so a 10% error in erosion shifts it by 400 m
    • Net gain is 1,000 m, and a small rate error cannot change it much
    • Net gain is 5,000 m, the larger total, whatever the erosion rate