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Related Concept Videos

Conditions on Early Earth02:06

Conditions on Early Earth

Around 4 billion years ago, oceans began to condense on earth while volcanic eruptions released nitrogen, carbon dioxide, methane, ammonia, and hydrogen into the primordial atmosphere. However, organisms with the characteristics of life were not initially present on earth. Scientists have used experimentation to determine how organisms evolved that could grow, reproduce, and maintain an internal environment.
The Colonization of Land02:22

The Colonization of Land

Changes in the environment of the early Earth drove the evolution of organisms. As prokaryotic organisms in the oceans began to photosynthesize, they produced oxygen. Eventually, oxygen saturated the oceans and entered the air, resulting in an increase in atmospheric oxygen concentration, known as the oxygen revolution approximately 2.3 billion years ago. Therefore, organisms that could use oxygen for cellular respiration had an advantage. More than 1.5 years ago, eukaryotic cells and...
Conditions on Early Earth02:06

Conditions on Early Earth

Around 4 billion years ago, oceans began to condense on earth while volcanic eruptions released nitrogen, carbon dioxide, methane, ammonia, and hydrogen into the primordial atmosphere. However, organisms with the characteristics of life were not initially present on earth. Scientists have used experimentation to determine how organisms evolved that could grow, reproduce, and maintain an internal environment.
Circular Orbits and Critical Velocity for Satellites01:16

Circular Orbits and Critical Velocity for Satellites

The Moon orbits around the Earth. In turn, the Earth (and other planets) orbit the Sun. The space directly above our atmosphere is filled with artificial satellites in orbit. One can examine the circular orbit, the simplest kind of orbit, to understand the relationship between the speed and the period of planets and satellites with respect to their positions and the bodies that they orbit.
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Thousands of artificial satellites orbit the Earth every day at various distances from the Earth. Satellites that orbit the Earth below an altitude of 1,600 km are considered to be orbiting in low-Earth orbit (LEO). Research satellites and Earth observation satellites are usually placed in LEO, and mostly orbit the Earth in elliptical orbits. Navigation satellites are placed in medium-Earth orbit (MEO), ranging from 2,000 km to 36,000 km from the surface of the Earth. Meanwhile, communication...
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Related Experiment Video

Updated: Jul 9, 2026

Simulation of the Planetary Interior Differentiation Processes in the Laboratory
06:04

Simulation of the Planetary Interior Differentiation Processes in the Laboratory

Published on: November 15, 2013

Tectonic evolution of the terrestrial planets.

J W Head, S C Solomon

    Science (New York, N.Y.)
    |July 3, 1981
    PubMed
    Summary

    Planetary tectonics vary due to lithosphere thickness and plate mobility. Understanding Venus

    Area of Science:

    • Planetary Science
    • Geology
    • Geophysics

    Background:

    • Tectonic styles and evolution vary significantly across terrestrial planets.
    • Plate tectonics, involving mantle recycling, is unique to Earth among terrestrial planets.
    • Other terrestrial planets like the Moon, Mars, and Mercury possess a single, immobile lithospheric shell.

    Purpose of the Study:

    • To investigate the factors influencing planetary lithospheric evolution and plate tectonics.
    • To evaluate the role of planetary size, chemistry, and heat sources in tectonic development.
    • To understand the tectonic evolution of Venus by comparing its features to Earth and smaller planets.

    Main Methods:

    • Comparative analysis of tectonic features across terrestrial planets.

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    Simulation of the Planetary Interior Differentiation Processes in the Laboratory
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    Published on: November 15, 2013

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    Surface Mapping of Earth-like Exoplanets using Single Point Light Curves
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  • Examination of factors such as lithospheric thickness, rheology, planetary size, chemistry, and heat sources.
  • Low-resolution surface mapping of Venus to identify geological features.
  • Main Results:

    • Vertical tectonic movements are similar across terrestrial planets, governed by local lithospheric thickness and rheology.
    • Venus exhibits a mix of tectonic features, including mountain belts and high plateaus (Earth-like) and possible impact basins (similar to smaller planets).

    Conclusions:

    • Planetary tectonic styles are fundamentally linked to lithospheric characteristics and mobility.
    • Further study of Venus' tectonic evolution is crucial for understanding the interplay of planetary size and chemistry in shaping geological processes.