Venus has more volcanism than previously known, new analysis finds
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[May 29, 2024]
By Will Dunham
WASHINGTON (Reuters) - Venus appears to be more volcanically active than
previously known, according to scientists whose new analysis of
decades-old radar images has spotted evidence of eruptions at two
additional sites on the surface of Earth's inhospitable planetary
neighbor.
Radar images obtained by NASA's Magellan spacecraft from 1990 to 1992
indicated large lava flows at these two locations in the Venusian
northern hemisphere at the time of the observations, the researchers
said. These findings, coupled with previous studies, indicate that the
planet's volcanic activity is comparable to Earth's, they added.
Magellan mapped 98% of the Venusian surface. Advances in computing
capability have made analyzing Magellan's radar data easier in recent
years.
"These findings significantly change our understanding of the degree to
which Venus is volcanically active, suggesting it could be much more
active than previously thought," said planetary scientist Davide
Sulcanese of d'Annunzio University in Pescara, Italy, lead author of the
study published this week in the journal Nature Astronomy.
One of the two sites is a volcano called Sif Mons, which is about 200
miles (300 km) wide and situated in a region called Eistla Regio. The
before-and-after radar images indicate a lava flow amounting to about 12
square miles (30 square km) of rock. The other site is a large volcanic
plain in a region called Niobe Planitia. About 17 square miles (45
square kilometers) of rock was produced in this lava flow.
"Both Sif Mons and the volcanoes in Niobe Planitia are shield volcanoes,
characterized by broad, gentle slopes formed by low-viscosity lava
flows," said d'Annunzio University planetary scientist and study
co-author Giuseppe Mitri.
The new rock at both locations was estimated to have an average depth
between about 10 and 66 feet (three and 20 meters).
"The lava flows observed along the western flank of Sif Mons exhibit
linear features with sinuous patterns that follow the direction of the
maximum slope, generally towards the west," said planetary scientist and
study co-author Marco Mastrogiuseppe of University Sapienza in Rome and
Link Campus University in Rome.
"Regarding the flows in Niobe Planitia, the lava flows appear to
originate near small shield volcanoes and extend towards the northeast,
also following the direction of the slope," Mastrogiuseppe added.
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A computer-generated 3D model of Venus' surface provided by NASA's
Jet Propulsion Laboratory shows the volcano Sif Mons which is
exhibiting signs of ongoing activity, in this undated handout image.
Using data from NASA's Magellan mission, Italian researchers
detected evidence of an eruption while the spacecraft orbited the
planet in the early 1990s. NASA/JPL/Handout via REUTERS
Venus is the second planet from the sun, and Earth the third. Venus
has a diameter of about 7,500 miles (12,000 km), slightly smaller
than Earth.
The new study builds on previous findings of ongoing Venusian
volcanic activity. A 2023 study found that a volcanic vent on Maat
Mons in a region called Atla Regio, near the equator, expanded and
changed shape during the Magellan mission.
"Our study is the first to provide direct proof of lava flows formed
during the Magellan mission period. By analyzing radar images from
the Magellan spacecraft, we observed changes in surface morphology
and radar data indicative of new lava flows," Sulcanese said.
"This offers direct evidence of ongoing volcanic activity on Venus,
building upon previous evidence such as atmospheric sulfur dioxide
variations, surface thermal emissions data, and especially the
evidence of deformation of a volcanic vent observed in Atla Regio,"
Sulcanese said.
Studying volcanic activity provides a fuller understanding of a
planet's internal heat and geological processes.
"It provides insights into the planet's thermal evolution, surface
renewal processes and atmospheric interactions," Mitri said.
The thick Venusian atmosphere, mainly carbon dioxide, traps in heat
in a runaway greenhouse effect, making Venus our solar system's
hottest planet.
"Despite Venus and Earth being very similar in terms of size, mass,
chemical composition and internal structure, there are fundamental
differences that make Venus an infernal planet," with a roasting
surface temperature and crushing atmospheric pressure, Sulcanese
said.
"The reason for this different evolution is still a subject of
debate," Sulcanese added, noting that planned NASA and European
Space Agency missions in the coming years "will help us better
understand why these two planets have met such different fates."
(Reporting by Will Dunham; Editing by Lisa Shumaker)
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