I saw these weird circular mounds in the ocean off the west coast of Scotland, and wondered what they were.

Turns out: they're extinct volcanoes, beveled flat by wind and waves, sunk deep beneath the sea. 🧵1/
Where did they come from? Look 1000 km to the NNW & you'll see Iceland - a region with not one, but two sources of volcanoes:

-> Atlantic Ocean spreading & associated decompression melting, and
-> A plume of hot material rising through the mantle.

2/

semanticscholar.org/paper/Geology-…
(Let's briefly admire what that volcanism looks like.) 🤩 🌋

3/

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/

doi.org/10.1016/j.epsl…
Track eruptions from that plume over time & you'll find volcanic rocks extending NW across Greenland, going back 70 million yrs.

And, because the plume is below a spreading center, a mirrored set to the SE - reaching our old volcanoes W of Scotland. 5/

steemit.com/geology/@soofl…
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/

researchgate.net/publication/23…
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/

oceanservice.noaa.gov/facts/light_tr…
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.

Download it here and explore! google.com/earth/versions/

10/end

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More from @JudithGeology

Mar 24
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/

Map source: deviantart.com/atlas-v7x
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/

ces.fau.edu/nasa/impacts/i…
Read 7 tweets
Mar 10
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.

2/

en.wikipedia.org/wiki/Hawaii_ho…
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/
Read 16 tweets
Mar 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/

theconversation.com/how-does-altit…
For comparison: the highest peak in the continental US is Mt. Whitney, at 14,494 feet (4418 m).

That's lower than the AVERAGE elevation of the Tibetan Plateau - a region 2000 km x 1000 km! 3/
Read 23 tweets
Jan 30
2.4 billion years ago, Earth's atmosphere was free of oxygen. Iron didn't rust! Only anaerobic species could survive.

And then ... cyanobacteria evolved photosynthesis, and began to pump oxygen into the atmosphere.

Oops.

🧵 1/n

#GreatOxygenationEvent

en.wikipedia.org/wiki/Great_Oxi… Image
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

#bandedironformations

en.wikipedia.org/wiki/Banded_ir… Image
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

#snowballEarth

theconversation.com/billions-of-ye…
Read 6 tweets
Jan 25
You might hear a geologist say: "We can't predict earthquakes."

Well, WHY NOT???

1/n

🧵⬇️⬇️⬇️

#earthquake #earthquakeprediction
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.

That's different from #forecasting, #earlywarning, and #aftershocks. 2/n

To date NO ONE has developed an effective way to predict significant earthquakes.

Issue #1: Faults are fractal.

"But we know where the tectonic plates are!"

Yes, mostly, but plate boundaries are complicated - see the maps below comparing plates vs. faults. 3/n

#tectoplot
Read 23 tweets
Jan 23
Oh, cool!

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.

But it's super hard to measure... 1/n
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!

rickallmendinger.net/faultkin

2/n
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

3/n

jgs.lyellcollection.org/content/162/1/… Image
Read 11 tweets

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