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9th grade Orbital cycles and ice ages worksheet

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Orbital cycles and ice ages

Grade 9 Science Worksheet

NameDate

Circle the best answer.

  1. Read this first

    EPICA Dome C temperature record (NOAA NCEI)

    Years agoTemperature vs last 1,000 years
    20,000−9.4 °C
    128,000+3.4 °C
    140,000−9.1 °C
    410,000+1.6 °C
    800,000−8.9 °C
  2. About how many 100,000-year ice-age cycles fit in 800,000 years, by Bo's math?

    • About 80
    • About 8
    • About 20
    • About 0.8
  3. A timeline divided into equal cycles. NASA: between 1 and 3 million years ago, ice ages came about every 41,000 years. About how many fit in that 2-million-year span, by Esme's math?

    • About 49
    • About 4.9
    • About 82
    • About 20
  4. Earth tilted more and less beside the Sun. NASA: the tilt was at its maximum about 10,000 years ago and reaches its minimum about 10,000 years from now. How does that span compare with the cycle, by Jun's math?

    • About 20,000 years, about half the 41,000-year cycle
    • About 10,000 years, a full cycle
    • About 41,000 years, a full cycle
    • About 20 years
  5. Orbit shape, tilt and wobble, each with its cycle. NASA: northern summers are about 4.5 days longer than winters today. Which cycle causes unequal season lengths, by Milo's reading?

    • Earth's daily spin
    • Eccentricity, the orbit's shape
    • Obliquity, the tilt of Earth's axis
    • Growing ice sheets
  6. EPICA Dome C temperature record (NOAA NCEI)

    Years agoTemperature vs last 1,000 years
    20,000−9.4 °C
    128,000+3.4 °C
    140,000−9.1 °C
    410,000+1.6 °C
    800,000−8.9 °C
  7. Using the EPICA table, how much warmer was 128,000 years ago than 140,000 years ago, by Noah's math?

    • About 125 °C
    • About 5.7 °C
    • About 3.4 °C
    • About 12.5 °C
  8. Using the EPICA table, how big was the change from 20,000 years ago (−9.4 °C) to the last 1,000 years, by Pia's math?

    • About 0.94 °C
    • About 9.4 °C colder in the last 1,000 years
    • About 18.8 °C
    • About 9.4 °C warmer in the last 1,000 years
  9. The table's 140,000- and 128,000-year values lie about 12,000 years apart. What does the change show, by Ren's reading?

    • A change within a single century
    • An interglacial warm period giving way to a new ice age
    • No change in climate
    • A glacial period giving way to a warm interglacial
  10. In 1976, Hays and colleagues tested Milankovitch's idea with deep-sea sediment cores (NASA). What did they find, by Tala's reading?

    • Orbital cycles matched major climate changes over 450,000 years
    • Tilt by itself explained each ice age, with no help from the other cycles
    • Ice ages came each year
    • Orbital cycles had no link to climate
  11. NASA: about 800,000 years ago ice-age cycles lengthened from 41,000 to 100,000 years. What do scientists say about why, by Zee's reading?

    • Precession came to an end
    • Several ideas exist, but there is no clear answer yet
    • It is fully explained
    • Earth's tilt stopped changing, so the cycle got longer
  12. Why can orbital changes that alter sunlight modestly still pace large ice ages, by Ari's reading (NASA)?

    • Ice absorbs more sunlight as it grows
    • Each ice age lasts a few years
    • Growing ice reflects more sunlight, adding more cooling
    • Orbital changes raise the Sun's output
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9th grade Orbital cycles and ice ages worksheet – printable
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About this worksheet

Explain how orbital cycles pace ice ages. Every version has 10 questions, and the answer key prints on the second page.

What your child will learn

  • I can name the three orbital cycles and their lengths: orbit shape about 100,000 years, tilt about 41,000 and wobble about 26,000 (25,771.5).
  • I can explain why tilt, not distance, sets the seasons, and why smaller tilt and cool summers let ice sheets build while growing ice adds cooling.
  • I can read signed values in the EPICA Dome C record and count cycles in a span of time.

Standard: HS-ESS2-4

Words to know

eccentricity: How stretched Earth's orbit is; cycles over about 100,000 years

obliquity: The tilt of Earth's axis; cycles over about 41,000 years

precession: The slow wobble of Earth's axis; about 25,771.5 years

perihelion: Earth's closest point to the Sun, around January 3

glacial: A cold stretch of an ice-age cycle, with large ice sheets

interglacial: A warm stretch between glacials

Common mistakes

Your child mixed up the cycles. NASA: orbit shape (eccentricity) about 100,000 years; tilt (obliquity) about 41,000; wobble (precession) about 26,000.

Your child misread the tilt's effect. NASA: a larger tilt makes seasons more extreme and favors melting; a smaller tilt gives cooler summers that let ice build up.

Your child tied the seasons to distance. NASA: Earth is closest to the Sun around January 3, during northern winter; tilt, not distance, sets the seasons.

Questions parents ask

What is the most common mistake with orbital cycles and ice ages?

Your child mixed up the cycles. NASA: orbit shape (eccentricity) about 100,000 years; tilt (obliquity) about 41,000; wobble (precession) about 26,000.

Are these 9th grade science worksheets free to print?

Yes. All 6 printable versions at each level are free to print, with the answer key, and no account is needed.

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