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9th grade How we know past climates: ice cores, tree rings, sediments worksheet

6 printable versionsBuilding Confidence10 questions · answer keyFree · no account

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How we know past climates: ice cores, tree rings, sediments

Grade 9 Science Worksheet - Building Confidence

NameDate

Circle the best answer.

  1. Read this first

    Use this

    Ice, a tree ring, a sediment layer and a pollen grain in a row.

  2. What are proxy data, by Ari's reading (NOAA)?

    • Satellite photos from the 1800s
    • Thermometer readings from millions of years ago
    • Preserved natural records that stand in for direct measurements
    • Forecasts of future weather
  3. Which of these is a proxy record of past climate, by Kira's reading (NOAA)?

    • Tomorrow's forecast
    • Tree rings
    • A modern weather-satellite photo
    • Today's rain-gauge reading
  4. Why do ice cores show yearly layers, by Jun's reading (NOAA)?

    • Summer and winter snow differ in texture and chemistry
    • Layers form from ocean waves
    • Each storm makes one yearly layer
    • Each layer is one century of snow
  5. What do the air bubbles in ice cores hold, by Luz's reading (NOAA)?

    Use the picture in question 3.

    • Ocean water
    • Tree pollen and nothing else
    • Samples of the past atmosphere's gases
    • Modern air pumped in by the drill during coring
  6. Use this

    Table, Ice-core CO₂ and Antarctic temperature (NOAA NCEI), with columns About how long ago, CO₂ in trapped air (ppm), Temperature vs last 1,000 years: 20,000 years, 194, −9.4 °C; 128,000 years, 276, +3.4 °C; 140,000 years, 193, −9.1 °C. Note: CO₂: Antarctic composite (Bereiter et al. 2015); temperature: EPICA Dome C (Jouzel et al. 2007); values rounded.

  7. Using the ice-core table, how much CO₂ did trapped air hold about 20,000 years ago, near the last ice age's peak, by Milo's reading (NOAA)?

    • About 425 ppm
    • About 276 ppm
    • About 9.4 ppm
    • About 194 ppm
  8. Ring widths of a rain-sensitive tree (model data)

    YearRing width
    19013 mm
    19021 mm
    19034 mm
  9. In temperate regions, how many rings does a tree usually add each year, by Noah's reading (NOAA)?

    • Ten
    • Two, one each season
    • One
    • One per decade
  10. A tree depends on rain in its growing season. What does a wide ring show, by Pia's reading (NOAA)?

    • A year when the tree did not grow
    • A cold, snowy winter
    • A wet year
    • A dry year
  11. What is cross dating, by Ren's reading (NOAA)?

    • Measuring the height of a tree
    • Counting the rings on a single stump by itself
    • Matching ring patterns in old wood to living trees to fix exact years
    • Matching tree rings to ice layers by color
  12. Use this

    Light oxygen moving from the sea into an ice sheet.

  13. Oxygen comes in light (oxygen-16) and heavy (oxygen-18) forms. Which evaporates slightly more easily, by Tala's reading (NASA)?

    • Neither one evaporates
    • Heavy oxygen-18
    • They evaporate equally
    • Light oxygen-16
  14. During ice ages, why is the ocean richer in heavy oxygen, by Zee's reading (NASA)?

    • Light oxygen gets locked away in the growing ice sheets
    • The cold ocean makes heavy oxygen
    • Plankton eat the light oxygen
    • Heavy oxygen is locked away in the growing ice sheets there
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9th grade How we know past climates: ice cores, tree rings, sediments worksheet – printable
Print: 123456

About this worksheet

Read past climates from ice cores, tree rings and sediments. Every version has 10 questions, and the answer key prints on the second page.

What your child will learn

  • I can explain what proxy data are and why we need them before the instrument record (about the 1800s).
  • I can date ice cores, tree rings and sediments by counting layers or using a deposition rate, and explain why deep ice layers are thin.
  • I can read oxygen isotopes (icy times leave heavy oxygen in the sea), ring widths and pollen, and explain why scientists compare several proxies.

Standard: HS-ESS2-4

Words to know

proxy data: Preserved natural records that stand in for direct measurements

ice core: A cylinder of ice drilled from an ice sheet, with yearly layers

cross dating: Matching ring patterns in old wood to living trees

isotope: A form of an element with a different mass, like oxygen-18

pack rat midden: A cemented pile of plants gathered by pack rats

resolution: How much short-term detail a record shows

Common mistakes

Your child treated proxies as direct measurements. NOAA: proxies are preserved natural records that stand in for measurements; instruments reach back only to about the 1800s.

Your child misread the layers. NOAA: ice cores and temperate trees usually add one layer or ring a year; deep ice layers get squeezed thinner.

Your child misread ring width. NOAA: trees limited by warmth grow wider rings in warm years; trees limited by moisture grow wider rings in wet years.

Questions parents ask

What is the most common mistake with how we know past climates: ice cores, tree rings, sediments?

Your child treated proxies as direct measurements. NOAA: proxies are preserved natural records that stand in for measurements; instruments reach back only to about the 1800s.

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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