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Geologic time scale and Moon

Shortcuts: Differences, Similarities, Jaccard Similarity Coefficient, References.

Difference between Geologic time scale and Moon

Geologic time scale vs. Moon

The geologic time scale (GTS) is a system of chronological dating that relates geological strata (stratigraphy) to time. The Moon is an astronomical body that orbits planet Earth and is Earth's only permanent natural satellite.

Similarities between Geologic time scale and Moon

Geologic time scale and Moon have 26 things in common (in Unionpedia): Age of the Earth, Ancient Greece, Aristotle, Atmosphere of Earth, Earth, Geology of the Moon, Giant-impact hypothesis, History of Earth, Imbrian, Jupiter, Late Heavy Bombardment, Lunar geologic timescale, Lunar mare, Mantle (geology), Moon, Natural satellite, Nectarian, Northern Hemisphere, Oxygen, Parts-per notation, Radioactive decay, Science (journal), Shen Kuo, Solar System, Stratigraphy, Sun.

Age of the Earth

The age of the Earth is 4.54 ± 0.05 billion years This age may represent the age of the Earth’s accretion, of core formation, or of the material from which the Earth formed.

Age of the Earth and Geologic time scale · Age of the Earth and Moon · See more »

Ancient Greece

Ancient Greece was a civilization belonging to a period of Greek history from the Greek Dark Ages of the 13th–9th centuries BC to the end of antiquity (AD 600).

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Aristotle

Aristotle (Ἀριστοτέλης Aristotélēs,; 384–322 BC) was an ancient Greek philosopher and scientist born in the city of Stagira, Chalkidiki, in the north of Classical Greece.

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Atmosphere of Earth

The atmosphere of Earth is the layer of gases, commonly known as air, that surrounds the planet Earth and is retained by Earth's gravity.

Atmosphere of Earth and Geologic time scale · Atmosphere of Earth and Moon · See more »

Earth

Earth is the third planet from the Sun and the only astronomical object known to harbor life.

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Geology of the Moon

The geology of the Moon (sometimes called selenology, although the latter term can refer more generally to "lunar science") is quite different from that of Earth.

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Giant-impact hypothesis

The giant-impact hypothesis, sometimes called the Big Splash, or the Theia Impact suggests that the Moon formed out of the debris left over from a collision between Earth and an astronomical body the size of Mars, approximately 4.5 billion years ago, in the Hadean eon; about 20 to 100 million years after the solar system coalesced.

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History of Earth

The history of Earth concerns the development of planet Earth from its formation to the present day.

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Imbrian

The Imbrian is a lunar geologic period divided into two epochs, the Early Imbrian and Late Imbrian.

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Jupiter

Jupiter is the fifth planet from the Sun and the largest in the Solar System.

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Late Heavy Bombardment

The Late Heavy Bombardment (abbreviated LHB and also known as the lunar cataclysm) is an event thought to have occurred approximately 4.1 to 3.8 billion years (Ga) ago, at a time corresponding to the Neohadean and Eoarchean eras on Earth.

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Lunar geologic timescale

The lunar geological timescale (or selenological timescale) divides the history of Earth's Moon into five generally recognized periods: the Copernican, Eratosthenian, Imbrian (Late and Early epochs), Nectarian, and Pre-Nectarian.

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Lunar mare

The lunar maria (singular: mare) are large, dark, basaltic plains on Earth's Moon, formed by ancient volcanic eruptions.

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Mantle (geology)

The mantle is a layer inside a terrestrial planet and some other rocky planetary bodies.

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Moon

The Moon is an astronomical body that orbits planet Earth and is Earth's only permanent natural satellite.

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Natural satellite

A natural satellite or moon is, in the most common usage, an astronomical body that orbits a planet or minor planet (or sometimes another small Solar System body).

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Nectarian

The Nectarian Period of the lunar geologic timescale runs from 3920 million years ago to 3850 million years ago.

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Northern Hemisphere

The Northern Hemisphere is the half of Earth that is north of the Equator.

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Oxygen

Oxygen is a chemical element with symbol O and atomic number 8.

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Parts-per notation

In science and engineering, the parts-per notation is a set of pseudo-units to describe small values of miscellaneous dimensionless quantities, e.g. mole fraction or mass fraction.

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Radioactive decay

Radioactive decay (also known as nuclear decay or radioactivity) is the process by which an unstable atomic nucleus loses energy (in terms of mass in its rest frame) by emitting radiation, such as an alpha particle, beta particle with neutrino or only a neutrino in the case of electron capture, gamma ray, or electron in the case of internal conversion.

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Science (journal)

Science, also widely referred to as Science Magazine, is the peer-reviewed academic journal of the American Association for the Advancement of Science (AAAS) and one of the world's top academic journals.

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Shen Kuo

Shen Kuo (1031–1095), courtesy name Cunzhong (存中) and pseudonym Mengqi (now usually given as Mengxi) Weng (夢溪翁),Yao (2003), 544.

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Solar System

The Solar SystemCapitalization of the name varies.

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Stratigraphy

Stratigraphy is a branch of geology concerned with the study of rock layers (strata) and layering (stratification).

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Sun

The Sun is the star at the center of the Solar System.

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The list above answers the following questions

Geologic time scale and Moon Comparison

Geologic time scale has 602 relations, while Moon has 544. As they have in common 26, the Jaccard index is 2.27% = 26 / (602 + 544).

References

This article shows the relationship between Geologic time scale and Moon. To access each article from which the information was extracted, please visit:

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