Every living thing on Earth — every plant, animal, and person — is built around the element carbon, which is why scientists call us “carbon-based life forms.” While we are alive, we take in a tiny amount of a radioactive version of carbon called Carbon-14. When we die, no more Carbon-14 gets in, and the atoms we already have start breaking down at a steady, predictable rate.

The “half-life” is how long it takes for half of those atoms to disappear. After one half-life, fifty percent of the original amount is left. After two half-lives, half of a half remains — only twenty-five percent of the original. The amount keeps shrinking, but the time between each halving stays the same — like cutting a piece of cake in half over and over every 5 minutes: the slices keep getting smaller, but the time between each cut never changes. Because that rate is so reliable, archeologists use math to turn “how much is left” back into “how long ago was this being alive?”

Rocks have a different clock: when magma cools deep underground, tiny crystals called zircon form, and they trap microscopic bits of uranium inside themselves. Over millions and even billions of years, that uranium slowly turns into lead. Before scientists figured out radioactive dating in the 1940s and 50s, archeologists had to guess at ages using how deep things were buried, the style of pottery nearby, or how thick tree rings were — methods that often resulted in uncertain estimates of the age of artifacts, with possible ranges in the thousands or even millions of years. Radiometric dating changed everything.

Reading Check · Fill in each blank using the word bank

Living cells are built using the element . While alive, plants and animals absorb a radioactive version of this element called . After something dies, no more enters its body, and the radioactive atoms inside slowly break apart. Scientists call the time it takes for half of those atoms to break down a . Very old rocks sometimes contain crystals of , and these crystals contain a different radioactive element, , that breaks down over a much longer timeline — over and even of years. Scientists can measure the amount of radioactive elements present and estimate how much they would originally contain. From the percentage still left, archeologists can estimate the age of artifacts with improved accuracy. Before this kind of dating was figured out in the , the age of artifacts was estimated only from clues like buried depth, pottery style, or tree rings.

Word Bank
carbon Carbon-14 half-life zircon uranium millions billions 1940s and 50s atoms nuclear
Methods of Estimating Age

Circle the methods that were used in the past to age artifacts and are still used today to confirm radioactive dating with multiple sources of data.

🔭Telescope
🌳Tree rings
🌡️Thermometer
🏺Pottery style
🧭Compass
⛰️Buried depth (soil layers)
Label the age of each artifact and rock
☀️ ☁️ ☁️ 🌳 🌲 🌳 SURFACE · RECENT Deer skull (demo) Age = years TOPSOIL · HOLOCENE Ishango Bone Age = years Ötzi the Iceman Age = years PLEISTOCENE Mammoth tusk Age = years MESOZOIC T. rex skull fossil Age = years Volcanic tuff Age = years PALEOZOIC Trilobite fossil Age = years Granite Age = years PRECAMBRIAN Acasta gneiss Age = years
Phrase / Word Bank
60,000 years 1 million years 5,730 years Carbon-14 Uranium-238 carbon zircon neither carbon-14 nor uranium-238 is 5,730 years is 4.468 billion years is long enough to detect a tiny remaining amount
Try Writing
To date an organic artifact (like the Ishango Bone or mammoth tusk), I use the probe, because the cells and tissues of living organisms are built with atoms.
To date a rock (like the granite or volcanic tuff), I use the probe, because the rock has crystals that contain that radioactive element.
A fossil — like the T. rex skull (where minerals replaced the bone) or the trilobite (an imprint pressed into sediment that became rock) — gives no signal because it contains .
Try Writing How did you estimate the age of the fossils?
How certain are you that your estimate is the exact age of the fossil? Why would this certainty be different from the others?
Tier 2 · General Academic Words
Tier 3 · Science Words