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Related Concept Videos

Cross-Sectional Research01:50

Cross-Sectional Research

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In cross-sectional research, a researcher compares multiple segments of the population at the same time. If they were interested in people's dietary habits, the researcher might directly compare different groups of people by age. Instead of following a group of people for 20 years to see how their dietary habits changed from decade to decade, the researcher would study a group of 20-year-old individuals and compare them to a group of 30-year-old individuals and a group of 40-year-old...
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Determining Relative Ages01:21

Determining Relative Ages

Determining Relative AgesGeologists determine the relative age of rock layers to understand Earth's history and the sequence of past events. Relative dating does not provide an exact numerical age but instead establishes the order of rock layers from oldest to youngest. Scientists use key principles of stratigraphy to determine relative ages, including:Law of Superposition – In an undisturbed sequence, the oldest rock layers are at the bottom, and the youngest are at the top.Principle of...
Geologic Time Scale01:11

Geologic Time Scale

Geologic Time ScaleThe geologic time scale is a system scientists use to describe the history of the Earth. It organizes Earth's 4.6-billion-year history into different periods based on major events like the formation of the planet, the appearance of life, mass extinctions, and the rise of new life forms. Studying the geologic time scale helps scientists understand how Earth and its life forms have changed over time and how different eras, periods, and epochs are connected through important...
Precambrian Continents01:29

Precambrian Continents

Precambrian ContinentsThe Precambrian period is the longest chapter in Earth’s history, covering almost 88% of the planet’s past. It started about 4.6 billion years ago, when Earth first formed, and lasted until around 541 million years ago. Back then, the world looked very different. There were no plants, no animals, and no oceans like we see today. The first continents started taking shape as molten rock cooled and hardened. These landmasses were small, unstable, and constantly changing...
Geologic Time Scale-II01:26

Geologic Time Scale-II

Geologic Time Scale-IIThe geologic time scale helps scientists understand Earth's history by organizing it into different time periods. The Mesozoic and Cenozoic Eras are the most recent and include major events such as the rise and fall of the dinosaurs, the formation of modern continents, and the emergence of mammals and humans. The Mesozoic Era included three periods: the Triassic, Jurassic, and Cretaceous. The Cenozoic Era is divided into the Paleogene Period and the Neogene Period.
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Sometimes we want to see how people change over time, as in studies of human development and lifespan. When we test the same group of individuals repeatedly over an extended period of time, we are conducting longitudinal research. Longitudinal research is a research design in which data-gathering is administered repeatedly over an extended period of time. For example, we may survey a group of individuals about their dietary habits at age 20, retest them a decade later at age 30, and then again...
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