Article 668XC Volcanic Eruptions May Have Caused the ‘Heat Death’ of Venus

Volcanic Eruptions May Have Caused the ‘Heat Death’ of Venus

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hubie
from SoylentNews on (#668XC)

Arthur T Knackerbracket writes:

https://www.extremetech.com/extreme/341085-volcanic-eruptions-may-have-caused-the-heat-death-of-venus

[...] The study points to Venus as an example, suggesting that a period of volcanic activity lasting millions of years may have turned it from a watery world into the inhospitable hellscape we see today.

Venus is considered Earth's sister world - the planets have similar sizes and densities, but the conditions on the surface could not be more different. The Venusian atmosphere is over 90 times denser than Earth's and composed mostly of carbon dioxide. The planet suffers from a runaway greenhouse effect with an average surface temperature of 864 degrees Fahrenheit (462 degrees Celsius).

The study focuses on the effects of "large igneous provinces," or LIPs, which are periods of widespread volcanic activity. On Earth, these conditions can last for thousands of years and have been responsible for more mass extinctions than asteroid impacts. LIPs can leave over 100,000 cubic miles of volcanic rock on the surface, but that's nothing compared with Venus, the surface of which is more than 80 percent solidified volcanic rock.

[...] Venus is a notoriously difficult planet to study. The only probes ever to reach the surface were destroyed by the crushing pressure and acidic clouds within minutes. NASA's upcoming missions may shed some light on the planet's history. DAVINCI (Deep Atmosphere Venus Investigation of Noble gases, Chemistry, and Imaging) will be able to map out the history of water on Venus, as well as how its climate changed over time. DAVINCI is currently scheduled to reach Venus toward the end of the decade. Next up will be the Venus Emissivity, Radio science, InSAR, Topography, And Spectroscopy (VERITAS) mission, an orbiter that will analyze the planet's surface.

Journal Reference:
M. J. Way et al 2022 Planet. Sci. J. 3 92 DOI: 10.3847/PSJ/ac6033

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