It is the time line, as well as we know it, for Earth's evolution. Each period is defined by a major geological or biological event. The first geologic time scale was proposed by British geologist Arthur Holmes (1890-1965) in 1913
Precambrian time (4567 to 542 mya)
· Hadean Eon (4567 to 3800 mya)
· Archaeon Eon (3800 to 2500 mya)
· Proterozoic Eon (2500 to 542 mya)
Phanerozoic Eon (542 mya to present)
· Paleozoic Era (542 mya to 251 mya)
o Cambrian Period (542 to 488.3 mya)
o Tommotion Stage (534 to 530 mya)
o Ordovician Period (488.3 to 443.7 mya)
o Silurian Period (443.7 to 416 mya)
o Devonian Period (416 to 359.2 mya)
o Carboniferous Period (359.2 to 299 mya)
o Mississippian Epoch (359.2 to 318.1 mya)
o Pennsylvanian Epoch (318.1 to 299 mya)
o Permian Period (299 to 251 mya)
· Mesozoic Era (251 to 65.5 mya)
o Triassic Period (251 to 199.6 mya)
o Jurassic Period (199.6 to 145.5 mya)
o Cretaceous Period (145.5 to 65.5 mya)
· Cenozoic Era (65.5 mya to today)
o Paleogene Period (65.5 to 23. 03 mya)
o Tertiary Period (65.5 to 2.58 mya)
o Paleocene Epoch (65.5 to 54.8 mya)
o Eocene Epoch (54.8 to 33.7 mya)
o Oligocene Epoch (33.7 to 23.03 mya)
· Neogene Period (23.03 mya to today)
o Miocene Epoch (23.03 to 5.3 mya)
o Pliocene Epoch (5.3 to 2.58 mya)
o Quaternary Period (2.58 mya to today)
o Pleistocent Epoch (2.58 mya to 11,400 yrs ago)
o Holocene Epoch (11,400 yrs ago to today)
The most recent Ice Age
A geological timeline helps scientists understand the history of Earth, including the formation of rocks, minerals, and the evolution of life. It helps us track major events, such as mass extinctions, climate changes, and the movement of continents, providing important insights into the planet's past and present conditions. By studying the timeline, researchers can make predictions about future geological events and better comprehend environmental changes.
You can find a timeline of Earth's ages in geological textbooks, scientific publications, or on reputable websites maintained by geological organizations or institutions. These timelines typically outline the major geological time periods, eras, and epochs spanning from the formation of Earth to the present day.
The geological or historical age refers to the time period during which certain events or processes occurred in Earth's history. It is determined based on the age of rocks, fossils, or other geological evidence found in a particular area. This information helps scientists understand the timeline of Earth's development and evolution.
Absolute chronology, which is the determination of exact dates or time periods. Geological chronology, which involves the study of the Earth's history based on geological events and formations. Astronomical chronology, which uses astronomical events and phenomena to establish a timeline.
A geological time scale is best reconstructed using a combination of radiometric dating, fossil evidence, and stratigraphic relationships between rock layers. By utilizing these methods together, scientists can create a comprehensive and accurate timeline of Earth's geological history.
Scientists may have challenges with pinpointing precise dates within geological time due to complex geological processes and the potential for radiometric dating to have margins of error. Additionally, gaps in the geological record can make it difficult to establish a continuous timeline of events. Interpreting the relative timing of different geological events can also be tricky, requiring careful analysis of rock layers, fossils, and other indirect evidence.
Scientists study geological time by analyzing rock layers and fossils to determine the relative ages of different formations. They also use radiometric dating techniques to assign numerical ages to specific events or objects in Earth's history. By combining these methods, scientists can create a detailed timeline of Earth's geological past.
it is a timeline that has multiple other timelines in it
A non-linear timeline.
a timeline of his life
It is a timeline about Jews of the past.