The ticking of a clock is constant, occurring at a steady rhythm/frequency.

While the decay of radioactive elements cannot be determined at a particular point in time, they do decay at a fairly steady rate over time. This allows you to statistically determine the rate at which a mass of radioactive material will steadily decay. So, the decay rate is steady, predictable, and follows a sort of rhythm over time just like the ticking of a clock.

The ticking of a clock is constant, occurring at a steady rhythm/frequency.

While the decay of radioactive elements cannot be determined at a particular point in time, they do decay at a fairly steady rate over time. This allows you to statistically determine the rate at which a mass of radioactive material will steadily decay. So, the decay rate is steady, predictable, and follows a sort of rhythm over time just like the ticking of a clock.

The ticking of a clock is constant, occurring at a steady rhythm/frequency.

While the decay of radioactive elements cannot be determined at a particular point in time, they do decay at a fairly steady rate over time. This allows you to statistically determine the rate at which a mass of radioactive material will steadily decay. So, the decay rate is steady, predictable, and follows a sort of rhythm over time just like the ticking of a clock.

The ticking of a clock is constant, occurring at a steady rhythm/frequency.

While the decay of radioactive elements cannot be determined at a particular point in time, they do decay at a fairly steady rate over time. This allows you to statistically determine the rate at which a mass of radioactive material will steadily decay. So, the decay rate is steady, predictable, and follows a sort of rhythm over time just like the ticking of a clock.

Their radioactive clock is set when they solidify from magma or lava.