How we know past climates: ice cores, tree rings, sediments
Grade 9 Science Worksheet - Challenge Me

Circle the best answer.
Ice, a tree ring, a sediment layer and a pollen grain in a row. A classmate says no one can know past climates because no one measured them. Which reply fits NOAA, by Esme's reading?
- No; thermometer records already reach back about 800,000 years in Antarctica
- Correct; thermometers are the one valid record
- No; satellites have watched for centuries
- No; ice cores, tree rings and sediments preserve climate signals
Read this first
Ring widths of a rain-sensitive tree (model data)
Year Ring width 1901 3 mm 1902 1 mm 1903 4 mm A student says a wide tree ring always means a warm year. Which reply fits NOAA, by Jun's reading?
- No; ring width shows the tree's age
- Correct; ring width tracks heat for each kind of tree in a forest
- Correct; wide rings mean cold years
- No; it depends on whether warmth or moisture limits that tree
Light oxygen moving from the sea into an ice sheet. A student says extra heavy oxygen in old sea shells means a warm time. Which reply fits NASA, by Kira's reading?
- No; light oxygen was locked in ice, so it was a cold, icy time
- Correct; the ice sheets were melting
- No; heavy oxygen means heavy rain
- Correct; warm water makes extra heavy oxygen build up in the shells
Model data: a lake gains about 1 mm of sediment a year. How many years does a 2.5 m core hold, by Milo's math?
- About 25,000 years
- About 2,500 years
- About 2.5 years
- About 250 years
The EPICA core reaches about 800,000 years over about 3,189 m (NOAA). About how many years per meter is that on average, by Noah's math?
Use the picture in question 4.
- About 0.004 years per meter
- About 25 years per meter
- About 2,500 years per meter
- About 250 years per meter
Four evidence cards, labeled A to D. Which evidence best supports a cold period about 20,000 years ago, by Pia's reading?
- A single pollen grain
- One wide tree ring
- Thermometer readings from that time
- Ice-core oxygen and sediment shells both point to more ice and colder air
Several proxy records lined up on one timeline. NOAA: long records tend to show less short-term detail. Which record best shows year-to-year changes over the last 500 years, by Ren's reading?
- The deepest section of an 800,000-year ice core
- A single pack rat midden
- A deep-sea core spanning millions of years
- A tree-ring record with one ring a year
Which summary of ice cores fits NOAA and NASA, by Zee's reading?
An ice core with yearly bands getting thinner with depth. An ice core with yearly bands getting thinner with depth. yearly bands trapped air bubbles depth - Less heavy oxygen in snow means warmer air
- Ice cores cover just the last century
- Each layer is a century, with no air inside
- Yearly layers, trapped air that records CO₂, and oxygen isotopes, reaching about 800,000 years back
Ring widths of a rain-sensitive tree (model data)
Year Ring width 1901 3 mm 1902 1 mm 1903 4 mm Which summary of tree rings fits NOAA, by Ari's reading?
- Rings cannot be dated
- Width tracks warmth for each species
- Two rings a year, and width shows age
- One ring a year; width tracks warmth or moisture; cross dating extends records
Ice, a tree ring, a sediment layer and a pollen grain in a row. Which summary of proxies fits NOAA, by Bo's reading?
- One proxy by itself gives the full picture
- Natural recorders, like ice, trees, sediments and pollen, extend records past instruments
- Thermometers from the distant past
- Forecast models of the future