(Let's briefly admire what that volcanism looks like.) 🤩 🌋
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So what does a double-volcano region 1000 km away have to do with a 50 million year old volcano? Mantle plumes are long-lived, & the one below Iceland is no exception. Here, you can see the slower velocity rock (i.e. hotter) below Iceland today. 4/
The volcanoes are long dead - last erupted 40-70 million yrs ago - but the mountains they left behind persist. Erosion is slow under water! These higher deeper halves remained undetected until the last century. 6/
At the base of the seamounts is 2 km deep seafloor in pure darkness. Life clusters around these highs (reaching 500-600 m depth), taking advantage of the relative proximity of light. This is the "twilight" zone of the ocean. 7/
Expeditions to one of the volcanoes - the Anton Dohrn seamount - found coral gardens, starfish, barnacles, sponges, lobsters and eels. This life is supported by the nutrient-rich water flowing up the steep sides of the seamount. 8/
So excess heat in the mantle caused eruptions tens of millions of years ago that created the conditions for a hidden garden of corals today far from the volcanic source.
And some weird bumps on the seafloor, mapped in Google Earth but invisible to people. 9/
It's almost hard to remember a time before Google Earth - the tools & data available for free for anyone curious about the Earth far outpace even the best data scientists could access 20 years ago.
I'm here to remind you that 20,000 years ago, sea level was ~130 m lower than today.
For Southeast Asia, that means that instead of isolated islands, the Sunda shelf was a vast landmass more than 1/2 the size of the continental USA. 🧵1/
This history of lower sea level defines the ecology of the region. Plants, animals, and people could move across regions now covered by open ocean.
Australia, however, was still separated by a wide archipelago called Wallacea - allowing it to maintain its own unique ecology. 2/
This didn't just happen once. The Ice AgeS are plural: cycles of rapidly rising then slowly falling temperatures, tracking atmospheric CO2 concentrations. As water froze into ice sheets, sea levels fell; when it melted, the oceans filled again. 3/
The Galápagos Islands aren't just cool because of Darwin and his finches - they're also a fascinating region geologically.
And the story that the geology and ecology tell together may be the most intriguing one of all.
🧵 1/
Like Hawaii, the Galápagos Islands are volcanic, formed above a plume of hot material rising in the mantle. That heat comes from radioactive material near the core-mantle boundary; hot material is low density, so it rises.
Active volcanoes form above the plume, but the volcanoes are carried away as the plate moves.
Hawaii may be small, but it's the tip of a massive mountain chain that runs for 3500 km, bends sharply north, & continues for 2500 km more. That rivals the length of the Andes! 3/
People sometimes talk about how the seafloor is one of the great unexplored mysteries - and it's true - but there's a vast region of land that also qualifies: the Tibetan Plateau. 🧵 1/
Standing at ~4.8 km above sea level (15,700 ft), the Plateau is extremely inhospitable to humans: oxygen is almost halved compared to sea level. Operating at this altitude is difficult: movement is exhausting, thinking is hard. 2/
Suddenly, iron dissolved in the oceans bonded with oxygen and precipitated, forming layers of rust on the ocean floor. The deposits got thicker and thicker, reaching 100s of meters. 60% of iron is mined from these layers! 2/n
Methane was no longer stable: it reacted with oxygen to form CO2. Methane is a far more powerful greenhouse gas - so dropping methane levels triggered sudden cooling. The Earth froze over, with glaciers reaching as far as the tropics. 3/n
First, let's define "prediction". A useful #earthquakeprediction will tell you where, when, and how big a significant #earthquake will be, with a reasonably high success rate.
Stress is basically how much the rocks are being squeezed, and in which direction. If we can know that, and also know how *strong* the rocks are, we can estimate whether they will break.
When rocks *do* break (#earthquake!), we can use that to estimate stress. If you know the direction of slip, you can do even better. This even works for earthquakes that occurred long ago, if they left scratches on the fault!
Or, if you have a lot of money and time, you can drill into the Earth and measure the orientation of maximum squeezing based on how the borehole deforms. #boreholebreakouts