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Geologists determine absolute age by comparing the amounts of radioactive and nonradioactive elements in ()rock. The radioactive, or ()
elements decay into nonradioactive elements. Because this
rate of decay is ()
for each element, geologists can compare the amounts of stable and unstable elements
to determine how much of the ()
elements have formed over time.

Geologists determine absolute age by comparing the amounts of radioactive and nonradioactive elements in igneous rock. The radioactive, or unstable elements decay into nonradioactive elements. Because this  rate of decay is constant for each element, geologists can compare the amounts of stable and unstable elements  to determine how much of the stable elements have formed over time.

Explanation:

The method used by geologists in calculating the precise or absolute age of a fossil is called radiometric dating. This calculation is done by measuring the amount of energy emitted by some radioactive elements present in the igneous rocks.

Each element with radioactive properties has a constant decay rate of its radiation, which is the amount of radioactivity that it loses over time. After the necessary time, the radioactive or unstable elements become stable particles.

Since each element has a constant decay rate, the time that has elapsed since its formation can be estimated.

Although fossils are normally found in sedimentary rock strata -which do not contain radioactive elements- their precise age is calculated using radiometric dating of adjacent igneous rock strata.

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Radiometric dating link

a. seed plant structure. 1. the three main plant organs are roots, stems, and leaves. a fourth kind of tissue, meristematic tissue, is responsible for plant growth. meristematic tissue is the only plant tissue that produces new cells by mitosis. plants can lose water out of their leaves as they exchange gases with the air

explanation:

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