Forces that build land up and wear it down

Grade 9 Science Worksheet

NameDate

Circle the best answer.

  1. Read this first

    Retreat of two layers (example data)

    LayerRockRetreat per 1,000 years
    Caphard limestone5 cm
    Columnsoft siltstone40 cm
  2. Bo projects 10,000 years ahead. How much further has the soft rock retreated than the cap, and what shape results?

    • 3.5 m further, leaving the column standing out beyond a worn-down cap above
    • 4 m further, leaving the cap overhanging the column
    • 35 cm further, leaving the cap overhanging the softer column below
    • 3.5 m further, leaving the cap overhanging the column as in a hoodoo
  3. Two mountain belts

    BeltHighest peak (m)Plate collision
    Himalayas8,849still pushing today
    Appalachians2,037ended over 250 million years ago
  4. Jun compares the belts. Which explanation of the height difference fits the table best?

    • Erosion piles sediment onto the Appalachian peaks, so they stay lower
    • Weathering is faster in the Himalayas, so it builds them higher
    • Uplift still feeds the Himalayas, while erosion has worn the Appalachians for over 250 million years
    • Both belts wear at the same rate, so just their starting heights differ
  5. Luz studies a cliff where nights often freeze and rock fragments pile at the base. Which observation best supports frost wedging as the main weathering?

    • A fan of sediment 5 km away at a river mouth
    • Rounded pebbles lying in a stream bed nearby
    • Rock faces coated with a soft, clay-rich crust
    • Sharp-edged fragments with fresh, unaltered faces piled at the cliff base
  6. Kira studies a field with 40 cm of soil. Weathering makes 0.05 mm of soil a year and erosion strips 0.2 mm (example data). If rates hold, how long until bare rock?

    • About 2,000 years
    • About 2,700 years
    • About 270 years
    • About 1,600 years
  7. Delta budget (example data)

    ItemAmount
    Sediment from the river12 million m³ a year
    Sediment removed by waves9 million m³ a year
    Delta area60 km²
  8. Milo spreads the net sediment evenly over the delta. By how much does its surface rise each year?

    • About 5 cm a year
    • About 20 cm a year
    • About 35 cm a year
    • About 0.5 cm a year
  9. Noah models a 2,000 m range that stops rising. Erosion lowers it 0.02 mm a year (example data). About how long until it is worn flat?

    • About 100 million years
    • About 100 billion years
    • About 100,000 years
    • About 10 million years
  10. Two Hawaiian islands

    IslandAge of oldest rockHighest point (m)Erupting now
    Kauaiabout 5 million years1,598no
    Hawaii (Big Island)under 1 million years4,207yes
  11. Ren compares the islands. Which explanation of their heights fits the table best?

    • Kauai is lower because lava did not build it; erosion did
    • Kauai is lower because it is younger than the Big Island
    • Lava still builds the Big Island up, while erosion has lowered Kauai for about 5 million years
    • The Big Island is higher because erosion has worn it more
  12. NPS gives the Grand Canyon's greatest depth as about 1,829 m, cut in 5–6 million years. Tala finds the average cutting rate in mm a year.

    • About 0.03 to 0.04 mm a year
    • About 3 to 3.7 mm a year
    • About 300 to 370 mm a year
    • About 0.30 to 0.37 mm a year
  13. Two ranges (example data)

    RangeClimateUplift (mm/yr)Erosion (mm/yr)
    Awet and freezing1.00.8
    Bdry and mild1.00.2
  14. Esme runs both ranges for 1 million years. Which range ends higher, and by how much?

    • Range A, by 600 m: wet, freezing air builds more rock
    • Range B, by 800 m: its own net gain over the period
    • Neither: they rise at the same rate, so they end equal
    • Range B, by 600 m: it gains 800 m while A gains 200 m
  15. Use this

    Table, Erosion rate as a range wears down (example data), with columns Time since uplift stopped, Height (m), Erosion rate (mm/yr): 0 years, 4,000, 1.0; 50 million years, 2,000, 0.3; 150 million years, 600, 0.05.

  16. Ari reads the table. Which explanation fits the falling erosion rate?

    • Erosion piles rock back onto the range, so less is removed
    • Lower, gentler slopes give water less energy to cut and carry rock
    • Lower ranges receive more sunlight, which slows erosion
    • Weathering stops once uplift stops, so nothing is left to carry away
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Forces that build land up and wear it down

Answer Key - Grade 9 Science Worksheet

Circle the best answer.

  1. Read this first

    Retreat of two layers (example data)

    LayerRockRetreat per 1,000 years
    Caphard limestone5 cm
    Columnsoft siltstone40 cm
  2. Bo projects 10,000 years ahead. How much further has the soft rock retreated than the cap, and what shape results?

    • 3.5 m further, leaving the column standing out beyond a worn-down cap above
    • 4 m further, leaving the cap overhanging the column
    • 35 cm further, leaving the cap overhanging the softer column below
    • 3.5 m further, leaving the cap overhanging the column as in a hoodoo
  3. Two mountain belts

    BeltHighest peak (m)Plate collision
    Himalayas8,849still pushing today
    Appalachians2,037ended over 250 million years ago
  4. Jun compares the belts. Which explanation of the height difference fits the table best?

    • Erosion piles sediment onto the Appalachian peaks, so they stay lower
    • Weathering is faster in the Himalayas, so it builds them higher
    • Uplift still feeds the Himalayas, while erosion has worn the Appalachians for over 250 million years
    • Both belts wear at the same rate, so just their starting heights differ
  5. Luz studies a cliff where nights often freeze and rock fragments pile at the base. Which observation best supports frost wedging as the main weathering?

    • A fan of sediment 5 km away at a river mouth
    • Rounded pebbles lying in a stream bed nearby
    • Rock faces coated with a soft, clay-rich crust
    • Sharp-edged fragments with fresh, unaltered faces piled at the cliff base
  6. Kira studies a field with 40 cm of soil. Weathering makes 0.05 mm of soil a year and erosion strips 0.2 mm (example data). If rates hold, how long until bare rock?

    • About 2,000 years
    • About 2,700 years
    • About 270 years
    • About 1,600 years
  7. Delta budget (example data)

    ItemAmount
    Sediment from the river12 million m³ a year
    Sediment removed by waves9 million m³ a year
    Delta area60 km²
  8. Milo spreads the net sediment evenly over the delta. By how much does its surface rise each year?

    • About 5 cm a year
    • About 20 cm a year
    • About 35 cm a year
    • About 0.5 cm a year
  9. Noah models a 2,000 m range that stops rising. Erosion lowers it 0.02 mm a year (example data). About how long until it is worn flat?

    • About 100 million years
    • About 100 billion years
    • About 100,000 years
    • About 10 million years
  10. Two Hawaiian islands

    IslandAge of oldest rockHighest point (m)Erupting now
    Kauaiabout 5 million years1,598no
    Hawaii (Big Island)under 1 million years4,207yes
  11. Ren compares the islands. Which explanation of their heights fits the table best?

    • Kauai is lower because lava did not build it; erosion did
    • Kauai is lower because it is younger than the Big Island
    • Lava still builds the Big Island up, while erosion has lowered Kauai for about 5 million years
    • The Big Island is higher because erosion has worn it more
  12. NPS gives the Grand Canyon's greatest depth as about 1,829 m, cut in 5–6 million years. Tala finds the average cutting rate in mm a year.

    • About 0.03 to 0.04 mm a year
    • About 3 to 3.7 mm a year
    • About 300 to 370 mm a year
    • About 0.30 to 0.37 mm a year
  13. Two ranges (example data)

    RangeClimateUplift (mm/yr)Erosion (mm/yr)
    Awet and freezing1.00.8
    Bdry and mild1.00.2
  14. Esme runs both ranges for 1 million years. Which range ends higher, and by how much?

    • Range A, by 600 m: wet, freezing air builds more rock
    • Range B, by 800 m: its own net gain over the period
    • Neither: they rise at the same rate, so they end equal
    • Range B, by 600 m: it gains 800 m while A gains 200 m
  15. Use this

    Table, Erosion rate as a range wears down (example data), with columns Time since uplift stopped, Height (m), Erosion rate (mm/yr): 0 years, 4,000, 1.0; 50 million years, 2,000, 0.3; 150 million years, 600, 0.05.

  16. Ari reads the table. Which explanation fits the falling erosion rate?

    • Erosion piles rock back onto the range, so less is removed
    • Lower, gentler slopes give water less energy to cut and carry rock
    • Lower ranges receive more sunlight, which slows erosion
    • Weathering stops once uplift stops, so nothing is left to carry away