Orbital cycles and ice ages
Grade 9 Science Worksheet

Circle the best answer.
Read this first
EPICA Dome C temperature record (NOAA NCEI)
Years ago Temperature 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 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
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
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
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
EPICA Dome C temperature record (NOAA NCEI)
Years ago Temperature 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 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
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
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
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
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
Why can orbital changes that alter sunlight modestly still pace large ice ages, by Ari's reading (NASA)?
Ice sheets reflecting sunlight back to space. Ice sheets reflecting sunlight back to space. Sun sunlight ice sheets space - 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

