M2 Subtopic 5 Flashcards
As sediments accumulate, they form distinct layers, each representing a different period in Earth’s history; are like pages in a book, with each layer telling a different part of Earth’s story
Stratification
are like pages in a book, with each layer telling a different part of Earth’s story
Stratified Rocks
Two Dating Methods
Relative and Absolute Dating
Establishes the sequence of events without determining their exact age. Used to understand the order in which layers and geological events occurred.
Relative Dating
In an undisturbed sequence of rock layers, the oldest layers are at the bottom, and the youngest are at the top.
This principle helps geologists identify the relative ages of different layers.
Principle of Superposition
Sedimentary layers are originally deposited in a horizontal position.
If layers are found tilted or folded, these changes occurred after deposition.
Principle of Original Horizontality
A rock or fault that cuts across other layers is younger than the layers it disrupts.
This principle is crucial for understanding the sequence of events that have affected rock formations.
Principle of Cross-Cutting Relationships
Fossils of organisms that lived during a specific, relatively short time frame.
Widely distributed and easily recognizable, making them ideal for correlating the age of rock layers across different regions.
Index Fossils
provides a precise numerical age for rocks and fossils.
This method is essential for calibrating the geological time scale and understanding the timing of specific events in Earth’s history.
Absolute Dating
measures the decay of radioactive isotopes within minerals to determine the exact age of rocks.
Widely used for dating igneous and metamorphic rocks and is key to determining the ages of ancient geological formations.
Radiometric Dating
the time it takes for half of the radioactive isotopes in a sample to decay
Half life
specific form of radiometric dating used to date organic materials, such as wood, bones, and shells.
Effective for dating materials up to about 50,000 years old.
Carbon Dating
organizes Earth’s history into a series of time intervals.
These subdivisions are based on significant events such as mass extinctions, major climate shifts, and the emergence of new life forms.
Geologic Time Scale
Subdivisions of Geologic Time
Eons, Eras, Periods, Epochs
The largest time units, encompassing billions of years. (Precambrian and Phanerozoic)
Eons