Time is the ongoing sequence of events that occur in an irreversible succession from the past through the present to the future. It is a measure of the duration between two events and is often represented using units such as seconds, minutes, hours, days, and years.
There are several units used to measure time:
Time can be measured using different instruments and methods, including:
Due to the Earth's rotation, different parts of the world experience daylight and darkness at different times. This has led to the establishment of time zones, which divide the world into 24 regions, each with its own standard time offset from Coordinated Universal Time (UTC).
In historical and geological contexts, time is often divided into eras, periods, and epochs to categorize and study the Earth's history and evolution. For example, the Paleozoic era represents a significant span of time in geological history.
Understanding time involves several key concepts: