Did Complex Life Appear Because the Magnetic Field was Weak?

Some parts of the history of the Earth's magnetic field are easy to measure. But the strength of the field is not one of them. We have lots of information of the reversals of the polarity of the field and the direction of the magnetism - think of the stripes on the ocean floor and knowing the latitude of when rocks were laid down - but the field strength of the field is harder to come by.

And this is important for the presence of the field is what protects us from deadly cosmic rays. It is very possible that no field = no life.

But some measurements of field strength have been made and one of the interesting things is that it was very low in the Ediacaran. It was a fifteenth of the present value. This and the consequences of this are discussed in THIS ARTICLE.

Did the reduction in magnetic field strength allow more genetic mutation in the single-celled creatures promoting the multi-celled Ediacaran fauna?

The article goes on to discuss the mechanism which affected the field, essentially the formation of the Earth's inner core. The 100 million years this took covers the Ediacaran and the "Cambrian Explosion".

The article gives a pleasing combination of Earth physics and biology. It may even be true!

Oceanic-plate Volcanism

The latest edition of NATURE GEOSCIENCE has several papers on the volcanism found on oceanic plates. This includes seamounts and vast drowned plateaus. The seamounts are often found in chains, but not every sea mount is in a chain. The magazine has a rather nice cover illustration.

This issue of Nature is reviewed in Earth-logs which has a more extensive version of the Nature cover.

3-D simulation of geodynamics beneath the Pacific and Indian Ocean floors. Credit: Hao Dong, Institute of Geology and Geophysics, Chinese Academy of Sciences.

The latest edition of Geology Bites - a podcast about all things geological - also focuses on seamounts, especially those in chains. The scientist interviewed is Bernhard Steinberger. I recommend looking at the website as well as listening to the podcast.

So there is a lot of interest in this subject at the moment. And I wish I could give a simple explanation of the conclusions of all this work.

I can't, but my minion, Google Gemini can! The Nature papers can be summarised as follows:-

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For decades, geologists used a simplified, step-by-step approach to map the Earth: volcanoes form over static "hot spots," plates move at ridges, and sink at subduction zones. However, recent studies published in Nature Geoscience show that the deep Earth is far more interconnected, messy, and dynamic than previously thought.

The key takeaways from the new research include:

"Seamount Breweries": Scientists used to think underwater volcanoes (seamounts) only formed in neat lines as a tectonic plate moved over a single, stationary "hot spot." However, most seamounts are scattered randomly. A new 290-million-year computer simulation explains why: massive, rising blobs of heat from deep near the Earth's core break apart as they hit the upper mantle. This creates wide, drifting "hot zones" that act like "breweries," popping up clusters of random volcanoes over time.

Deep Earth Launchpads: Volcanoes are much more common on ocean floors that have drifted over huge, super-hot structures at the very bottom of the Earth's mantle (called LLSVPs). These deep structures act like permanent engines launching heat upward.

The Connected Domino Effect: Massive volcanic plateaus, like the Ontong Java Plateau in the Pacific, didn't just form from a simple hot plume. New models suggest that about 130 million years ago, a sudden increase in plates sinking (subducting) around the edges of the Pacific Ocean forced the Earth's interior to rearrange. This slowed down sea-floor spreading at the ridges, forcing intense heat to escape elsewhere—melting dense, old crust deep down and pouring out unprecedented amounts of magma onto the deep ocean floor.

The Big Picture Change:

Geology is moving away from looking at isolated puzzle pieces. Instead, scientists now view the entire planet as a single, connected web where a change in one area (like a sinking tectonic plate) instantly triggers a massive reaction somewhere else (like a giant underwater volcanic eruption thousands of miles away).

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And the Geology Bites podcast can be reduced to:-

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In this Geology Bites podcast episode, geophysicist Bernhard Steinberger discusses whether mantle hotspots (the deep plumes of hot rock that feed volcanic chains like Hawaii) are truly stationary.

His research and modeling lead to several key conclusions about mantle dynamics, plate tectonics, and how we map ancient Earth:

1. Hotspots Are Not Fixed

For decades, scientists assumed hotspots were stationary anchors that could be used as a fixed frame of reference to measure tectonic plate movement. Steinberger’s core conclusion is that hotspots actively move. They are bent and blown sideways (advected) by the massive mantle convection currents they must rise through—similar to smoke bending in a breeze.

2. The Famous "Hawaiian-Emperor Bend" Required Two Things

The striking, sharp 60-degree bend in the Hawaii-Emperor seamount chain (formed around 47 million years ago) was long thought to be caused solely by a sudden change in the Pacific plate's direction. Paleomagnetic data and Steinberger’s models show a dual reality:

• The Hawaii hotspot itself was drifting rapidly southward (at about 3.5 cm per year) before 47 million years ago and then slowed or shifted.

• The sharpness of the bend required both a change in plate motion and a change in the hotspot's own drift coinciding at the same time.

3. Hotspots Move Independently

Hotspots do not move together as a rigid grid. Each one drifts at its own speed and direction (typically around 1 cm per year) depending on its local mantle environment. For example, while the Hawaii hotspot was moving southward, its South Pacific neighbor, the Louisville hotspot, was drifting slowly eastward. This independent movement is the definitive proof that they are not fixed relative to each other.

4. Why Hotspots Stay Relatively Anchored

Despite this movement, hotspots change position slowly enough to still be highly useful. Whole-mantle seismic tomography reveals why: the plume conduits are incredibly thick (several hundred kilometers across) and rooted in dense, sluggish thermochemical piles (LLSVPs) right at the core-mantle boundary. Because the lower mantle moves so slowly, the roots of these plumes stay relatively stable.

5. A "Moving Hotspot Reference Frame" is Necessary

Because we cannot treat hotspots as completely stationary, geophysicists must use Steinberger's mantle-flow models to calculate past hotspot drift. By factoring in this drift alongside paleomagnetic data (which tracks a plate's latitude relative to Earth's spin axis), scientists can establish a more accurate "moving hotspot reference frame" to reconstruct how tectonic plates moved relative to the deep mantle over hundreds of millions of years.

6. The Whole Lithosphere Drifts Westward

When you sum up the total movement of all tectonic plates within this deep-mantle reference frame, the entire outer shell of the Earth (the lithosphere) exhibits a net westward rotation of about 1.5 cm per year at the equator. Steinberger concludes that this isn't caused by tidal forces from the Moon, but is simply driven by the massive Pacific plate being dragged rapidly westward by subduction zones along its edges.

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 Sea Floor Spreading Observed!

A correspondent has sent me THIS LINK. It records what people thought must be happening but which no one had actually measured! 

It is the result of the installation of measuring equipment on the axis of the Southeast Indian Ridge (SEIR) - a mid Ocean ridge - and on the Amsterdam transform fault (TF). Both are not very far from Amsterdam Island. This is one of the most inaccessible places on Earth. It is about mid way between Western Australia and South Africa. To the south is Antarctica.

The article goes into a vast amount of detail which I will not attempt to interpret. Google Gemini was asked to rewrite the abstract in easy to understand language and came up with the following:-

Scientists have captured a rare, up-close look at the ocean floor literally tearing itself apart and forming new crust.

Because mid-ocean ridges (underwater mountain ranges where tectonic plates pull apart) are buried deep underwater, they are incredibly hard to monitor. However, researchers had equipment perfectly placed in the Indian Ocean to catch a massive "rifting event" right as it started on April 26, 2024.

Here is what happened over the span of about 16 days:

• The Ground Opened Up: An underground magma chamber deflated, sending channels of liquid rock (called dykes) bursting sideways through the ridge.

• The Sea Floor Shifted: The valley floor sank by 4 meters (about 13 feet) and widened by more than a meter.

• A Massive Eruption occurred: The magma broke through the surface, spilling roughly 160 million cubic meters of lava onto the ocean floor.

• Silent Earthquakes Cleared a Mystery: Tectonic plates usually move with a lot of shaking, but this event triggered a lot of "aseismic slip"—meaning the ground slid smoothly without causing measurable earthquakes.

Why this matters: Scientists have always wondered why mid-ocean ridges have far fewer earthquakes than expected. This discovery suggests that underground magma movements actually lubricate the faults, letting the tectonic plates slide past each other quietly and smoothly rather than violently snapping.

Studying the Hadean is Difficult!

For a start there is not much of it! Perhaps 20km² on Hudson Bay. Most studies have concentrated on zircon grains found in younger rocks. The best that can be said is that there was felsic magma and water was about. 

But there are other approaches. The early Earth was characterised by impacts from space, but direct evidence of these is missing on the Earth. The surface of the moon however records these and scaling up to the size of the Earth indicates that they would have a major influence on the Hadean on the Earth.

This is considered in THIS ACADEMIC PAPER and is summarised in this ARTICLE. The conclusion reached is that the heat produced from the kinetic energy of the impacts would have made almost everything start to melt. Below 3.5km lots of rocks of all kinds would be melting. Above 3.5km heat loss to space would keep things relatively cool.

The Earthlogs article is well worth reading. It may be easier to understand if you read the following summary produced by Google Gemini.

The Hadean Eon (~4.6 to 4.0 billion years ago) lacks a substantial rock record, leaving geologists to rely heavily on the geochemical signatures of rare, tiny zircon grains. To shed light on this elusive era, researcher Tim Johnson and his colleagues modeled the impacts of heavy celestial bombardment on the early Earth, scaling up lunar cratering data to account for Earth's greater gravitational pull.

The study reveals that during the Hadean, the energy released by frequent asteroid impacts significantly outweighed internal radiogenic heat generation. This intense, fluctuating external energy profoundly altered Earth’s thermal dynamics. Rather than shedding heat through modern plate tectonics and mantle convection, the Hadean Earth relied on massive, rapid melting events. Magma transported immense heat directly to the surface, allowing energy to radiate into space—the most efficient planetary cooling mechanism.

The team’s modeled geotherm indicates that temperatures increased rapidly with depth. Beneath a depth of just 3.5 kilometers, the uppermost Hadean crust was in a partially molten state. At depths exceeding 10 kilometers, between 40% and 70% of basaltic crust would have been liquefied. This pervasive melting effectively nullified the traditional distinction between brittle and ductile rock behaviors.

Consequently, the simulation rules out the existence of a rigid lithosphere or stabilizing plate tectonics during this period. Instead, the Hadean mantle was dominated by chaotic, high-energy convection. This continuous recycling of early granitic and continental crust into a literal melting pot perfectly explains the near-total absence of intact Hadean rocks today. This volatile cycle of impact-driven tectonics only ceased around 3.9 to 3.8 billion years ago, when the heavy bombardment subsided and allowed stable, modern planetary geology to emerge.

 The Lizard - Origin and Emplacement

I came across THIS ARTICLE just this morning and have not had a chance to study it in any depth. As I will not be writing in the blog  for several weeks, and the article will be of interest to many of you, here is a short summary written by Google Gemini:-  

This article details the formation, subduction, and obduction of the Mid-Devonian Lizard ophiolite within the Variscan orogenic belt of Cornwall, SW England.

Key Findings and Geological History:

Ophiolite Structure and Origin: The Lizard ophiolite represents a nearly intact thrust slice of oceanic crust (dated via U-Pb zircon to ~386.8 Ma, Givetian) and upper mantle. It originally formed above a south-dipping subduction zone within the Rheic Ocean.

Metamorphic Sole: Situated at the base of the ophiolite is an amphibolite-to-greenschist facies metamorphic sole (~395 Ma, late Emsian). This sole is intruded by the Kennack Igneous Complex, a suite of granitoids reflecting the partial melting of diverse protoliths during subduction and subsequent obduction.

Underlying Thrust Sheets: Mechanically underlying the ophiolite is a complex mélange unit alongside the heavily folded and faulted Middle Devonian to Carboniferous sedimentary rocks of the Dodman, Veryan, and Carrick thrust sheets.

Tectonic Progression: Tectonic shortening propagated from the south-southeast (SSE) to the north-northwest (NNW). This structural push progressively emplaced distal Gramscatho Group rocks onto the passive continental margin of Avalonia (Laurussia).

Post-Collisional Activity: Following initial crustal shortening, the region experienced Late Carboniferous to Early Permian extensional reactivation and subsequent crustal melting, culminatng in the widespread intrusion of the Cornubian granites between 295 and 275 Ma.

The paper highlights that the overall tectono-stratigraphy, metamorphic sole development, and underlying thrust architectures of the Lizard ophiolite share distinct geological parallels with the iconic Semail ophiolite in Oman.

 Down to Earth Extra June 2026

The June 2026 edition of Down to Earth Extra has been published. You can download it HERE or you can read it below.

 The Earth's Core Changes Direction

But Does it Matter? THIS ARTICLE caught the attention of a correspondent who forwarded the link to me (Thank You!). It concerns the flow of the molten iron which forms the outer core of the Earth. The outer core starts at a depth of 2,890km and is 2,260km thick. It is thought to be 80 to 85% iron, about 5% nickel and the rest is a mix of lighter elements like sulphur, oxygen, silicon and carbon.

It is the outer core which generates the Earth's magnetic field and this keeps cosmic radiation out. This is a good thing! And it is the study of the magnetic field which tells us the direction the core is moving. For a long time it was thought that a gentle western drift of 10 to 40 km per year (1mm per second) was normal. 

But in 2010, the bit under the Pacific, started moving eastwards. This continues but has slowed since 2020. What caused this is unknown and the change was unexpected. Perhaps there is more happening in the core than we know about!

Does it matter? Probably not - the Earth's magnetic field is still doing its job and shows no sign of turning off. 

The academic paper on which the article is based will be found HERE

The End of the Dinosaurs

THIS ARTICLE in The Conversation gives a minute by minute account of what happened when the asteroid struck. And it tells how the impact led to the death of the dinosaurs and the rise of the mammals. And it is co-written by Mike Benton and Monica Grady, so it is most probably correct! (At least at the time of writing.)

The article is well worth reading. If you are content with a summary, below is Google Gemini's.

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The Immediate Aftermath (T+0 to 5 Minutes)

The asteroid, traveling faster than the speed of sound, hit the Yucatán Peninsula with the force of billions of Hiroshima bombs. If you were within 1,000 miles, you didn't hear the impact; you were vaporized by the thermal radiation before the sound waves could even reach you.

Within minutes, supersonic winds—stronger than any Category 5 hurricane—flattened entire forests. The atmosphere briefly turned into an oven, reaching temperatures of over 200°C (400°F).

The Environmental Collapse (T+1 Hour to 1 Week)

As the crust rebounded from the impact, it formed a crater 30 kilometres deep, launching molten rock into space. This material rained back down as "impact spherules," igniting global wildfires.

Then came the "stinky" phase. The asteroid hit a region rich in sulphur, blasting massive amounts of it into the sky. Combined with the smoke from burning forests and decaying carcasses, the entire planet likely smelled like rotting vegetables and acrid smoke.

The Long Winter

The soot and sulphur created a global shroud, blocking the sun for years. Photosynthesis stopped. The oceans became acidic from nitrogen oxides, and the planet plunged into a deep freeze.

It is a humbling reminder of our planet’s fragility. While this Armageddon wiped out the giants, it left a tiny opening for small, burrowing mammals—our ancestors—to survive. Without that terrible Tuesday, humans might never have had the chance to walk the Earth.

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A Visualisation by Google Gemini

This visualization focuses on the global environmental shift. The sky is no longer blue but choked with thick, black soot and sulphate aerosols. This dense layer blocks the sun, plunging the planet into darkness. The illustration visualizes the "smell" described in the research by depicting the air itself as a visual fog of acid rain, illuminated by the low, dim, hellish glow of widespread global wildfires.

 Volcanic Items of Interest

Various items have come to my notice lately so here they are in no particular order.

• Can volcanic eruptions be forecast, like the weather? The origin of this was THIS ARTICLE and the answer is no but we are getting better at it. What controls volcanism is not easily visible and is not active all the time, unlike weather which is visible and happening constantly. The article covers many aspects of volcanism and has some spectacular photographs.
  
  
• Is the Campi Flegrei in Naples going to erupt? The Campi Flegrei to the west of downtown Naples is used to low grade volcanic activity - earthquake swarms, ground uplift and subsidence - there is a state of emergency but not yet at a level which would trigger mass evacuation. 
  
  
  Earthquakes detected in Campi Flegrei area, Italy from February 15 - 18, 2025. Credit: INGV
  
  
  
  
  
  
• Are Extinct Volcanoes actually Dormant? This comes from THIS ARTICLE. And the evidence for this comes from the "extinct" Methana volcano not far from Athens. It seems that zircon crystals formed throughout the volcanoes history, including during long periods of quiescence. Are they still forming now?
  
  

  

  
  

  The Southern Aegean Volcanic Arc, showing Methana on the left and Santorini at the bottom. (Giorgostr/Wikimedia Commons)
  
  

  
  
• Lots of magma under Tuscany. Tuscany is not known for volcanism but recent seismological studies have indicate that Yellowstone volumes of magma lie 10km under the surface. The academic paper detailing this is HERE. 

 Would You be Scared of this Giant Octopus?

Generally octopuses don't fossilise - they are essentially bags of water. But their beaks are preserved and someone has found some big ones in Cretaceous rocks. And using present day beak sizes and octopus sizes has come to the conclusion that their beaks belonged to an octopus 7 to 19 metres in length!

Cretaceous marine predators (at maximum estimated size) with a scuba diver for scale. Credit: After Ikegami et al. Fig. 4, and Jacobs 2026.

Was the octopus a top predator or was it an extra large food source for a Mosasaurus? It is certainly a very good focus for speculation. Proving anything might be a difficult task.

You can read all about it HERE, based on THIS PAPER

 Some New (but Old) Cambrian Fossils

A correspondent sent me THIS LINK (but I had spotted it my self!). It concerns a recently discovered Lagerstätte in Southern China, called the Huayuan biota.

It has an added importance as being just after the first mass extinction of the Phanerozoic. It contains some old favourites from the Burgess Shale but many new species have been identified.

The find is of importance for many reasons but for me it is important for the wonderful photographs of the beasties. The source academic paper is HERE

non-bilaterian metazoans and deuterostomes from the Huayuan biota

 How and Why Etna is Unusual

A correspondent sent me THIS LINK. It is based on THIS ACADEMIC PAPER. Both links are quite complex and the best summary of them can be provided by Chat GPT.

The GA will visit Etna this June and I will be there! I look forward to hearing what degree of complexity we hear when we are on the slopes!

Here is ChatGPT's summary.

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The article explains how scientists may finally understand the unusual behaviour of Mount Etna, one of the world’s most active and puzzling volcanoes. Although Etna is over 500,000 years old and sits above a subduction zone where tectonic plates collide, its eruptions don’t match typical volcanic models. Instead of producing the kinds of magma expected in such settings, Etna frequently emits alkaline lava more typical of hotspot volcanoes like those in Hawaii—despite no hotspot being present nearby.

To solve this mystery, researchers analysed the chemistry of Etna’s lava over hundreds of thousands of years. They found that its composition has remained remarkably consistent, even as surrounding tectonic conditions changed. This suggests the magma feeding Etna is not newly formed each time, as in most volcanoes, but instead comes from a long-lasting, stable source deep underground.

The study proposes that Etna is fed by pockets of magma trapped about 80 kilometres beneath the Earth’s surface, in a region between the upper mantle and tectonic plates. As the African Plate moves beneath the Eurasian Plate, pressure squeezes this stored magma upward through cracks in the crust, much like water from a sponge.

This mechanism resembles that of so-called “petit-spot” volcanoes—small volcanic features usually found on the ocean floor. However, Etna is vastly larger, making it an unusual and possibly unique example of this process operating on a massive scale.

These findings reshape scientists’ understanding of how volcanoes can form and function, suggesting Etna may not fit into standard categories. The research also has practical importance, helping improve assessments of volcanic hazards in nearby populated areas such as Catania and Messina.

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 The Hunga-Tonga Eruption Hid its Effect

A correspondent sent me THIS LINK. It concerns the 1922 eruption of Hunga-Tonga. This occurred under water and this had the effect of disguising its impact. 

The release of sulphur dioxide (SO₂) is often used to measure the cooling affect of eruptions, but Hunga-Tonga released little SO₂ to the atmosphere. And therefore it was assumed that it had little affect on the climate. The SO₂ released reacted with sea water - I assume sulphuric acid will be somewhere in the reactants.

But the lack of SO₂ in the atmosphere does not mean that the eruption had little climactic affect. 3 billion tons of water vapour went into the atmosphere in 1 hour! And it went very high - into the stratosphere and mesosphere. And there it had complex climatic results.

Read the article to understand some of the complexities!

 Another Huge Eruption Sometime (Geologically) Soon

A correspondent has sent me THIS LINK concerning a volcano which produced the largest eruption of the Holocene. Recent research indicates that the magma chamber is slowly refilling.

When one considers the damage the Holocene eruption did to what was then a sparsely populated area - just south of Japan's southernmost large island, Kyushu - another similarly sized eruption today would be catastrophic. Population densities are rather higher nowadays!

The researchers have found that the magma refilling the magma chamber is new stuff - not the leftovers of the last eruption.

You can get a better idea of the article by reading a summary provided by ChatGPT.

The article describes new research into the Kikai Caldera, a largely submerged volcano Japan responsible for one of the most powerful eruptions in Earth’s recent geological history. Around 7,300 years ago, the volcano produced the Akahoya eruption—the largest known eruption of the Holocene—ejecting vast quantities of material, spreading ash across Japan and beyond, and likely devastating the ancient Jōmon population.

Although the volcano has remained relatively quiet since then, scientists have now discovered that its  magma chamber is slowly refilling. Using advanced seismic techniques, including air-gun pulses and ocean-bottom seismometers, researchers mapped the subsurface structure beneath the caldera. Their results reveal a large magma reservoir that appears to be the same system responsible for the ancient eruption. 

Importantly, the magma currently accumulating is not simply leftover material from the previous eruption. Chemical analysis shows it is newly injected magma, indicating an active replenishment process. This is supported by evidence of a lava dome forming within the caldera over the past several thousand years, suggesting continuous magmatic activity.

The findings provide insight into how giant caldera systems “recharge” over long timescales. Researchers propose a model in which fresh magma is gradually injected into shallow reservoirs, eventually rebuilding the conditions necessary for another large eruption. This mechanism may apply not only to Kikai but also to other major volcanic systems such as Yellowstone and Toba.

While there is no indication of an imminent eruption, the study highlights the importance of monitoring such systems. Given today’s dense populations, even a moderate eruption could have severe consequences. Ultimately, the research aims to improve understanding of volcanic cycles and enhance the ability to detect warning signs well before future catastrophic eruptions occur.

Can Volcanoes be Connected?

 Can Volcanos be Connected?

A correspondent has sent me THIS ARTICLE. For ever geologists have thought that volcanoes could be studied in isolation but, more recently it has been discovered that magma does not just travel towards the surface but can also go sideways - it can move from one volcano to another, sometimes many kilometres apart. And, sometimes the type of rock erupted can change - which seems very odd.

Iceland’s Fagradalsfjall fissure system erupted multiple times between 2021 and 2023, after which the Svartsengi fissure system seemed to take its place.

The article in Quanta Magazine (which has some wonderful photos) describes, at length, coupled volcanos. I recommend reading it. I attach a summary produced by ChatGPT.

The Quanta Magazine article “When Coupled Volcanoes Talk, These Researchers Listen” explores a growing realization in volcanology: volcanoes are not always isolated systems, but can be physically connected and interact through shared underground magma pathways. By tracking how magma moves between volcanoes, scientists are uncovering “conversations” between volcanic systems that could improve eruption forecasting and deepen understanding of Earth’s interior dynamics.

The article begins with the famous 1912 eruption in Alaska involving Mount Katmai and the Novarupta vent. For decades, scientists assumed Katmai itself erupted and collapsed after expelling its magma. However, later geological mapping revealed that the eruption actually occurred about 10 kilometres away at Novarupta, which had effectively drained magma from Katmai. This discovery provided early evidence that magma can move laterally across significant distances, linking separate volcanic structures.

Modern research has expanded on this idea, showing that such connections are not rare. Advances in monitoring technologies—such as seismometers that detect magma movement and satellite-based measurements of ground deformation—allow scientists to track magma migration in near real time. These tools reveal that magma does not always rise vertically, as once assumed, but can flow sideways through complex subterranean networks.

A key focus of current research is Iceland’s Reykjanes Peninsula, where volcanic systems appear to operate in sequence. After eruptions at one fissure system, activity can shift to another nearby system, suggesting that magma is redistributed underground. This behaviour gives the impression that volcanoes are “talking” to each other—when one system quiets down, another becomes active. Such patterns indicate that volcanic regions may function as interconnected networks rather than independent vents.

Scientists are now attempting to map these hidden magma pathways and understand the physical mechanisms behind them. Magma behaves like a complex fluid mixture, with its viscosity depending on composition—silica-rich magma is thicker, while low-silica magma flows more easily. These properties influence how magma travels through the crust and how it links different volcanic systems.

Understanding these connections has practical importance. If magma can shift from one volcano to another, monitoring a single volcano in isolation may be insufficient for predicting eruptions. Instead, researchers must consider entire volcanic regions as integrated systems. By identifying patterns of magma transfer, scientists hope to anticipate where eruptions might occur next, even if the triggering signals originate elsewhere.

Ultimately, the research highlights a shift in how volcanologists conceptualize volcanic behaviour—from isolated eruptions to dynamic, networked systems. By “listening” to how volcanoes interact through shared magma, scientists are developing a more nuanced and predictive understanding of volcanic activity. This approach could lead to better hazard assessments and earlier warnings for communities living near active volcanic regions.

 

 What Caused the Younger Dryas

The Younger Dryas was a cold period which started 12,870 years ago. The last glacial maximum had finished about 20,000 years ago, so there had been about 7,000 years when things had been getting warmer. At 12,870 years ago thing got cooler quickly - in Europe the average temperature dropped 6⁰C in just 3 years! I suspect this would make life difficult for the people in the area. This cooling lasted for 1,170 years.

The causes of this are discussed in THIS ARTICLE, partially based on this JOURNAL ARTICLE, and this MAGAZINE ARTICLE. Possible culprits include:

1. A meteor strike
   
   
2. Drainage from a large glacial lake, disrupting the North Atlantic Drift.
   
   
3. An unknown volcanic eruption. (But not the Laacher See eruption - wrong trace elements and a bit later than the start of the Younger Dryas.)

There is evidence of volcanism at the start of the Younger Dryas. Where it was is still unknown. But the meteor strike is now discounted. We are left with culprits 2 and 3. And they do not rule each other out.

Below I attach a summary of the article which started this post, produced by ChatGPT.

The Earth-logs article argues that the long-debated cause of the Younger Dryas cold interval—an abrupt return to near-glacial conditions about 12,870 years ago—is now effectively resolved. The Younger Dryas interrupted the gradual warming that followed the last Ice Age, with temperatures in parts of the Northern Hemisphere dropping dramatically within just a few years and remaining cold for over a millennium.

Historically, several explanations have competed. One popular idea was that a massive influx of freshwater into the North Atlantic disrupted ocean circulation, particularly the Gulf Stream, reducing heat transport to higher latitudes. Another controversial hypothesis proposed that a comet or asteroid impact triggered the cooling, but this has largely been rejected due to lack of reproducible evidence.

The Earth-logs post highlights newer geochemical and ice-core evidence that points instead to a major volcanic trigger. Ice cores from Greenland show a pronounced sulphate spike at the onset of the Younger Dryas, indicating a very large volcanic eruption. While the well-known Laacher See eruption in Germany occurred around the same time, its scale and chemical signature do not match the observed sulphate anomaly. This implies that a much larger, as yet unidentified eruption injected vast quantities of aerosols into the atmosphere.

Such an eruption would have rapidly reduced incoming solar radiation, causing sharp cooling. Crucially, this initial volcanic cooling could have pushed the climate system past a tipping point, weakening ocean circulation and locking the Northern Hemisphere into a prolonged cold state. In this view, volcanism acted as the trigger, while feedbacks within the ocean–atmosphere system sustained the millennium-long chill.

The article concludes that this combined explanation—a large volcanic event initiating a cascade of climatic feedbacks—best fits the available evidence. It reconciles the abrupt onset seen in ice cores with the extended duration of the Younger Dryas, offering a coherent solution to a long-standing geological puzzle.

 Down to Earth Extra April 2026

The April 2026 edition of Down to Earth Extra has been published. you can download it HERE or you can read it below.

Subducted Slabs - Where and How

Earth-Logs, one of this blogs favourite sources has come up with an interesting article which you can find HERE. It is based on THIS ARTICLE which will appear in a Nature Journal soon.

It concerns subducting plates and what happens to them. It is thought that mineral density changes are the main control, but the authors of the paper suggest that another control is viscosity changes caused by cooler slabs entering the mantle. Their paper is summarised below (by ChatGPT) and further summarised in the diagram at the bottom of this page.

This is fascinating stuff but all the evidence is gained at a distance and we will never get there. So we have to be content with speculating about phase changes and viscosity. But these are the best explanations we have for the observations we make.

Seismic tomography does not support the idea that oceanic slabs sink intact all the way to the core–mantle boundary. Instead, many slabs stall and accumulate at depths around 660 km and 1000 km. The 660 km boundary is reasonably explained by pressure-driven mineral changes (especially in olivine) that increase density and resist further sinking. However, no equivalent mineral transition explains stagnation at ~1000 km depth.

Recent research by Jing Li and colleagues proposes that variations in mantle viscosity, rather than just mineral density changes, control slab behaviour. Their combined experimental and modelling work suggests that as slabs descend, they trigger recrystallization in the surrounding mantle, reducing grain size and creating localized low-viscosity zones. These zones can either facilitate or hinder slab movement, leading to complex, uneven descent.

They identify four subduction modes depending on trench retreat speed and mantle properties:

• Slow retreat + low-viscosity patches → slabs penetrate past 660 km but stagnate at ~1000 km
• Slow retreat + uniform mantle → slabs buckle between 660–1000 km
• Fast retreat (with or without low-viscosity zones) → slabs stagnate at ~660 km

The study also suggests that older, “fossil” slabs may weaken the mantle and create low-viscosity regions that influence later subduction. These processes help explain seismic observations and imply that the mantle is highly heterogeneous.

Overall, the findings highlight that mantle dynamics are complex, with past tectonic activity influencing present-day plate motion, deep mantle convection, plume formation, and the chemical diversity of mantle-derived magmas.

 The Silverpit - an Impact Structure

A correspondent brought THIS ARTICLE to my attention. It is based on THIS ACADEMIC PAPER.

I am getting up to speed with Artificial Intelligence (AI) and used ChatGPT to summarise the Science Daily article. I think it did a pretty good job. 

(I am using this free, Bristol University, COURSE to further my knowledge of AI. It seems pretty good so far.)

A recent study has provided strong new evidence that the Silverpit structure beneath the southern North Sea was created by an asteroid impact rather than by geological processes such as salt movement. The feature, first identified in seismic survey data collected during North Sea oil exploration in the early 2000s, had long been debated among geologists. Researchers from Heriot-Watt University have now used improved seismic imaging together with mineral analysis to support the impact interpretation.

According to the study, the impact occurred about 43–46 million years ago, during the Eocene epoch. Scientists estimate that the asteroid responsible was roughly 160 metres in diameter. When it struck the seabed, the collision released immense energy, excavating a large crater and ejecting vast quantities of rock and sediment into the surrounding environment. Seismic data reveal circular structures typical of impact craters, while rock samples show signs of shock metamorphism—microscopic changes in mineral structure produced by extremely high pressures, which are characteristic of meteorite impacts.

The consequences of the collision would have been dramatic. The impact likely generated a massive tsunami, possibly exceeding 100 metres in height, that would have spread across the ancient North Sea basin. Such a wave could have flooded nearby coastlines and significantly altered local landscapes. The event would also have produced a large plume of debris, water, and vapour thrown high into the atmosphere.

For years, many scientists suggested the Silverpit feature might instead be the result of salt tectonics, a process in which underground salt layers move and distort surrounding sediments. The new combination of geophysical and mineralogical evidence, however, provides the clearest support yet for the impact hypothesis.

By confirming the origin of the Silverpit crater, the research adds another entry to the record of asteroid impacts on Earth. It also highlights that significant ocean impacts capable of generating large tsunamis have occurred within relatively recent geological time.

 Down to Earth Extra March 2026

The March 2026 edition of Down to Earth Extra has been published. You can download it HERE or you can read it below.