Dating Volcanic Eruptions on Venus
I write the Eruptions blog on Big Think. I've been mesmerized with volcanoes (and geology) all my life. It helps that part of my family comes from the shadow of Nevado del Ruiz in Colombia, where I could see first hand the deadly effects of volcanic eruptions. Since then, I've taken a bit of a winding path to become a volcanologist. I started as a history major at Williams College, almost went into radio, but ended up migrating to geology, including an undergraduate thesis on Vinalhaven Island, Maine. I followed this up by changing coast to get my Ph.D. from Oregon State University. Then I ran a MC-ICP-MS lab at University of Washington for a spell (and wrote for an indie rock website). I spent three years as a postdoctoral scholar at University of California - Davis studying the inner workings of magmatic systems. I am now an assistant professor at Denison University and have projects in New Zealand, Chile and Oregon.
I am fascinated by volcanoes, their eruptions and how those eruptions interact with the people who live around the volcanoes. I started this blog after getting frustrated with the news reports of volcanic eruptions. Most of them get the information wrong and/or are just sensationalistic. I will try to summarize eruptions as they occur, translate some of the volcanic processes that are happening and comment on the reports themselves.
And no matter what people tell you, I definitely do not have a cat named Tephra. (OK, I do).
You can find out more about my research by visiting my website. If you have any comments, questions or information, feel free to contact me at eruptionsblog at gmail dot com.
(Note: Look for updates on Merapi and Kliuchevskoi later today)
I caught an article over the weekend about the potential of recent volcanism on Venus. The study that appeared Geophysical Research Letters found that some flows on the surface of Venus are, in fact, still warm enough to be recognized as, well, warmer than the surrounding surface (see upper left - click on image to see a larger version). Dr. Nataliya Bondarenko and her colleagues looked at microwave data from the Magellan mission during the 1990s - and using this data, relative and absolute heat flow on the surface can be compared. A few of the flows on the Bereghinia Planitia (see below) appear to be much warmer than the surrounding - up to 85C above the the expected temperature.
Image of the Bereghinia Planitia on Venus, a potential location of recent volcanism on Venus.
So, why is this interesting? Well, remember, after lava erupts, it cools, but not instaneously. The residual heat from the lava (magma) takes time to dissipate - entirely through conduction. This means that if there is anomalously high temperatures recorded on features that look like lava flows, this would suggest that the flows could be geologically recent. Bondarenko suggests that the heat measured on these flows on Venus could mean that they are less than a century old, otherwise the flows would not have appeared "hot" to the Magellan microwave instruments. The flow is at least 15 years old as it was imaged by Pioneer Venus in 1978, but this could means that the flow is anywhere from 15-100 years old, making it the youngest extraterrestrial silicate magmatism in the solar system.
There have been other studies on the age of lava flows on Venus. A paper in Science by Suzanne Smrekar and others looked at the ages of flows in the southern hemisphere of Venus. They used geomorphic criteria - the extent of weathering on the flows - to determine potential ages. They found that the flows are no less than 2.5 million years old, but likely closer to 250,000 years or less rather than the centuries old that Bondarenko found.
Beyond this, there is little other corroborating evidence for volcanic activity on Venus. Last year, there was some interesting anomalies in the atmosphere of Venus (discovered by an amateur astronomer) that could be interpreted as a volcanic plume, but it was never substantiated as an eruption.
The surface of Venus imaged by Magellan radar.
The surface of Venus does obviously show evidence of geologically recent volcanism - the surface of Venus is covered with features such as lava flows, fissures and domes that likely formed within the last half a billion years based on the extent of cratering on the surface of the planet. In fact, there are some theories that suggest that the entire surface of Venus (see above) was formed during a catastrophic volcanic event that enveloped much of the surface about 300 million years ago and since then, only 4-6% of the surface has been resurfaced. However, much of the evidence of this is circumstantial and is not universally accepted. It is clear, though, that the volcanic activity on Venus is likely linked to the harsh climate of the planet.
Evidence of explosive volcanism on the surface of Venus.
The Magellan mission captured multitude of amazing images of the volcanic features on Venus, including the famous pancake domes and evidence for explosive eruptions (see above) on the surface as well. If any planet in the solar system is likely to have a silicate eruption in the (geologically) near future, it is the Earth's sister planet.
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