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#magma — Public Fediverse posts

Live and recent posts from across the Fediverse tagged #magma, aggregated by home.social.

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  1. What with various volcanoes deciding to act up recently and therefore being in the news, I thought it was a good time to compare geology and politics.

    #USPol #magma #geology #politics #MAGA #RockStupid #volcano

  2. What with various volcanoes deciding to act up recently and therefore being in the news, I thought it was a good time to compare geology and politics.

    #USPol #magma #geology #politics #MAGA #RockStupid #volcano

  3. What with various volcanoes deciding to act up recently and therefore being in the news, I thought it was a good time to compare geology and politics.

    #USPol #magma #geology #politics #MAGA #RockStupid #volcano

  4. What with various volcanoes deciding to act up recently and therefore being in the news, I thought it was a good time to compare geology and politics.

    #USPol #magma #geology #politics #MAGA #RockStupid #volcano

  5. What with various volcanoes deciding to act up recently and therefore being in the news, I thought it was a good time to compare geology and politics.

    #USPol #magma #geology #politics #MAGA #RockStupid #volcano

  6. WHAT’S ON THE SHELF, AUGUST 26TH – INDEPENDENT PUBLISHERS
    What’s on the Shelf is built from distributor order forms and shipping date information, giving fans a heads-up on what may be landing at their...
    comiccrusaders.com/comics/comi
    #08262026 #comic books #comics #Ignition Press #independent #Indie #Indie Comics #kodansha #mad cave #magma #Manga #ncbd #New Comic Book Day #New Comics #oni #viz #what's on the shelf

  7. WHAT’S ON THE SHELF, AUGUST 26TH – INDEPENDENT PUBLISHERS
    What’s on the Shelf is built from distributor order forms and shipping date information, giving fans a heads-up on what may be landing at their...
    comiccrusaders.com/comics/comi
    #08262026 #comic books #comics #Ignition Press #independent #Indie #Indie Comics #kodansha #mad cave #magma #Manga #ncbd #New Comic Book Day #New Comics #oni #viz #what's on the shelf

  8. Passing overhead a few minutes ago 👀

    #ABD7746 #CC7746 Magma Aviation, operated by Air Atlanta Icelandic
    Boeing 747-481(BCF), TF-AMP

    570mph at 34,000ft (6.4 miles)
    Routing Liege to Chicago

    #aviation #photography #b747 #magma

  9. Passing overhead a few minutes ago 👀

    #ABD7746 #CC7746 Magma Aviation, operated by Air Atlanta Icelandic
    Boeing 747-481(BCF), TF-AMP

    570mph at 34,000ft (6.4 miles)
    Routing Liege to Chicago

    #aviation #photography #b747 #magma

  10. Passing overhead a few minutes ago 👀

    #ABD7746 #CC7746 Magma Aviation, operated by Air Atlanta Icelandic
    Boeing 747-481(BCF), TF-AMP

    570mph at 34,000ft (6.4 miles)
    Routing Liege to Chicago

    #aviation #photography #b747 #magma

  11. Passing overhead a few minutes ago 👀

    #ABD7746 #CC7746 Magma Aviation, operated by Air Atlanta Icelandic
    Boeing 747-481(BCF), TF-AMP

    570mph at 34,000ft (6.4 miles)
    Routing Liege to Chicago

    #aviation #photography #b747 #magma

  12. Passing overhead a few minutes ago 👀

    #ABD7746 #CC7746 Magma Aviation, operated by Air Atlanta Icelandic
    Boeing 747-481(BCF), TF-AMP

    570mph at 34,000ft (6.4 miles)
    Routing Liege to Chicago

    #aviation #photography #b747 #magma

  13. WHAT’S ON THE SHELF, AUGUST 19TH – INDEPENDENT PUBLISHERS
    What’s on the Shelf is built from distributor order forms and shipping date information, giving fans a heads-up on what may be landing at their...
    comiccrusaders.com/comics/comi
    #08192026 #comic books #comics #Ignition Press #independent #Indie #Indie Comics #kodansha #mad cave #magma #Manga #ncbd #New Comic Book Day #New Comics #oni #viz #what's on the shelf

  14. WHAT’S ON THE SHELF, AUGUST 19TH – INDEPENDENT PUBLISHERS
    What’s on the Shelf is built from distributor order forms and shipping date information, giving fans a heads-up on what may be landing at their...
    comiccrusaders.com/comics/comi
    #08192026 #comic books #comics #Ignition Press #independent #Indie #Indie Comics #kodansha #mad cave #magma #Manga #ncbd #New Comic Book Day #New Comics #oni #viz #what's on the shelf

  15. Un “latido” bajo Etiopía podría partir a África en dos

    Si tiene solo unos segundos, lea estas líneas: Bajo la región etíope de Afar, el material caliente del manto asciende en pulsos que debilitan, poco a poco, la corteza terrestre, según un nuevo estudio publicado en Nature Geoscience. El análisis de más de 130 muestras de rocas volcánicas reveló un “adelgazamiento localizado” de la corteza: […]
    The post Un “latido” bajo Etiopía podría partir a África en dos appeared first on CR Hoy.

    #Afar #Ciencia #Egipto #Magma #Océanos #VisualA3

    crhoy.com/un-latido-bajo-etiop

  16. Un “latido” bajo Etiopía podría partir a África en dos

    Si tiene solo unos segundos, lea estas líneas: Bajo la región etíope de Afar, el material caliente del manto asciende en pulsos que debilitan, poco a poco, la corteza terrestre, según un nuevo estudio publicado en Nature Geoscience. El análisis de más de 130 muestras de rocas volcánicas reveló un “adelgazamiento localizado” de la corteza: […]
    The post Un “latido” bajo Etiopía podría partir a África en dos appeared first on CR Hoy.

    #Afar #Ciencia #Egipto #Magma #Océanos #VisualA3

    crhoy.com/un-latido-bajo-etiop

  17. Un “latido” bajo Etiopía podría partir a África en dos

    Si tiene solo unos segundos, lea estas líneas: Bajo la región etíope de Afar, el material caliente del manto asciende en pulsos que debilitan, poco a poco, la corteza terrestre, según un nuevo estudio publicado en Nature Geoscience. El análisis de más de 130 muestras de rocas volcánicas reveló un “adelgazamiento localizado” de la corteza: […]
    The post Un “latido” bajo Etiopía podría partir a África en dos appeared first on CR Hoy.

    #Afar #Ciencia #Egipto #Magma #Océanos #VisualA3

    crhoy.com/un-latido-bajo-etiop

  18. Un “latido” bajo Etiopía podría partir a África en dos

    Si tiene solo unos segundos, lea estas líneas: Bajo la región etíope de Afar, el material caliente del manto asciende en pulsos que debilitan, poco a poco, la corteza terrestre, según un nuevo estudio publicado en Nature Geoscience. El análisis de más de 130 muestras de rocas volcánicas reveló un “adelgazamiento localizado” de la corteza: […]
    The post Un “latido” bajo Etiopía podría partir a África en dos appeared first on CR Hoy.

    #Afar #Ciencia #Egipto #Magma #Océanos #VisualA3

    crhoy.com/un-latido-bajo-etiop

  19. Massive Magma Reservoir Discovered Beneath Tuscany

    📰 Original title: A colossal magma system has been hiding beneath Tuscany

    🤖 IA: It's clickbait ⚠️
    👥 Users: It's clickbait ⚠️

    View full AI summary en.killbait.com/massive-magma-

    #science #magma #seismic

  20. Massive Magma Reservoir Discovered Beneath Tuscany

    📰 Original title: A colossal magma system has been hiding beneath Tuscany

    🤖 IA: It's clickbait ⚠️
    👥 Users: It's clickbait ⚠️

    View full AI summary en.killbait.com/massive-magma-

    #science #magma #seismic

  21. Massive Magma Reservoir Discovered Beneath Tuscany

    📰 Original title: A colossal magma system has been hiding beneath Tuscany

    🤖 IA: It's clickbait ⚠️
    👥 Users: It's clickbait ⚠️

    View full AI summary en.killbait.com/massive-magma-

    #science #magma #seismic

  22. Massive Magma Reservoir Discovered Beneath Tuscany

    📰 Original title: A colossal magma system has been hiding beneath Tuscany

    🤖 IA: It's clickbait ⚠️
    👥 Users: It's clickbait ⚠️

    View full AI summary en.killbait.com/massive-magma-

    #science #magma #seismic

  23. WHAT’S ON THE SHELF, AUGUST 5TH – INDEPENDENT PUBLISHERS
    What’s on the Shelf is built from distributor order forms and shipping date information, giving fans a heads-up on what may be landing at their...
    comiccrusaders.com/comics/comi
    #08052026 #comic books #comics #Ignition Press #independent #Indie #Indie Comics #kodansha #mad cave #magma #Manga #ncbd #New Comic Book Day #New Comics #oni #viz #what's on the shelf

  24. WHAT’S ON THE SHELF, AUGUST 5TH – INDEPENDENT PUBLISHERS
    What’s on the Shelf is built from distributor order forms and shipping date information, giving fans a heads-up on what may be landing at their...
    comiccrusaders.com/comics/comi
    #08052026 #comic books #comics #Ignition Press #independent #Indie #Indie Comics #kodansha #mad cave #magma #Manga #ncbd #New Comic Book Day #New Comics #oni #viz #what's on the shelf

  25. Anatomy Of A Seafloor Spreading Event Captured By In Situ Seismogeodesy
    --
    doi.org/10.1038/s41586-026-107 <-- shared paper
    --
    smithsonianmag.com/smart-news/ <-- shared technical media article
    --
    H/T @Seabed 2030
    “🔍 For the first time, scientists have observed seafloor spreading in real time.
    Seafloor spreading is the process by which new oceanic crust is formed at mid-ocean ridges - a geological process that has shaped entire ocean basins over millions of years.
    During a research expedition in the Indian Ocean, scientists had just deployed a suite of instruments when a series of earthquakes triggered a seafloor spreading event, allowing them to observe the process as it unfolded.
    The findings offer rare new insights into how new oceanic crust forms and how the seafloor continues to evolve…”
    --
    “Earth’s outermost layer - the crust - is constantly renewing itself. It’s broken into giant chunks called tectonic plates that pull apart, push against or slide past one another, creating grand geologic features.
    Underwater mountain ranges, or mid-ocean ridges, for instance, generally take shape where two tectonic plates are moving away from each other. Magma can then bubble up in between, solidifying and turning into new oceanic crust as part of a process called seafloor spreading. Although the phenomenon has created entire ocean basins, it remains quite mysterious because it happens so deep in the water.
    Now, for the first time, scientists have observed this dynamic activity happening in real time. They describe their findings - and their stroke of luck - in a study [link above], shedding light on a mechanism that made roughly two-thirds of Earth’s crust…”
    --
    #Seabed2030 #OceanMapping #Hydrospatial #remotesensing #seafloor #seafloorspreading #oceanic #crust #geology #structuralgeology #IndianOcean #earthquake #midoceanridge #instrumentation #marine #seabed #hydrography #model #modeling #mapping #GIS #spatial #tectonicplates #magma #fortuitous #survey #seismogeodetic #monitoring #submarine #rifting #observation #volcanism #seismicity #dyke #fault #faulting #midoceanridge #MOR

  26. Anatomy Of A Seafloor Spreading Event Captured By In Situ Seismogeodesy
    --
    doi.org/10.1038/s41586-026-107 <-- shared paper
    --
    smithsonianmag.com/smart-news/ <-- shared technical media article
    --
    H/T @Seabed 2030
    “🔍 For the first time, scientists have observed seafloor spreading in real time.
    Seafloor spreading is the process by which new oceanic crust is formed at mid-ocean ridges - a geological process that has shaped entire ocean basins over millions of years.
    During a research expedition in the Indian Ocean, scientists had just deployed a suite of instruments when a series of earthquakes triggered a seafloor spreading event, allowing them to observe the process as it unfolded.
    The findings offer rare new insights into how new oceanic crust forms and how the seafloor continues to evolve…”
    --
    “Earth’s outermost layer - the crust - is constantly renewing itself. It’s broken into giant chunks called tectonic plates that pull apart, push against or slide past one another, creating grand geologic features.
    Underwater mountain ranges, or mid-ocean ridges, for instance, generally take shape where two tectonic plates are moving away from each other. Magma can then bubble up in between, solidifying and turning into new oceanic crust as part of a process called seafloor spreading. Although the phenomenon has created entire ocean basins, it remains quite mysterious because it happens so deep in the water.
    Now, for the first time, scientists have observed this dynamic activity happening in real time. They describe their findings - and their stroke of luck - in a study [link above], shedding light on a mechanism that made roughly two-thirds of Earth’s crust…”
    --
    #Seabed2030 #OceanMapping #Hydrospatial #remotesensing #seafloor #seafloorspreading #oceanic #crust #geology #structuralgeology #IndianOcean #earthquake #midoceanridge #instrumentation #marine #seabed #hydrography #model #modeling #mapping #GIS #spatial #tectonicplates #magma #fortuitous #survey #seismogeodetic #monitoring #submarine #rifting #observation #volcanism #seismicity #dyke #fault #faulting #midoceanridge #MOR

  27. Anatomy Of A Seafloor Spreading Event Captured By In Situ Seismogeodesy
    --
    doi.org/10.1038/s41586-026-107 <-- shared paper
    --
    smithsonianmag.com/smart-news/ <-- shared technical media article
    --
    H/T @Seabed 2030
    “🔍 For the first time, scientists have observed seafloor spreading in real time.
    Seafloor spreading is the process by which new oceanic crust is formed at mid-ocean ridges - a geological process that has shaped entire ocean basins over millions of years.
    During a research expedition in the Indian Ocean, scientists had just deployed a suite of instruments when a series of earthquakes triggered a seafloor spreading event, allowing them to observe the process as it unfolded.
    The findings offer rare new insights into how new oceanic crust forms and how the seafloor continues to evolve…”
    --
    “Earth’s outermost layer - the crust - is constantly renewing itself. It’s broken into giant chunks called tectonic plates that pull apart, push against or slide past one another, creating grand geologic features.
    Underwater mountain ranges, or mid-ocean ridges, for instance, generally take shape where two tectonic plates are moving away from each other. Magma can then bubble up in between, solidifying and turning into new oceanic crust as part of a process called seafloor spreading. Although the phenomenon has created entire ocean basins, it remains quite mysterious because it happens so deep in the water.
    Now, for the first time, scientists have observed this dynamic activity happening in real time. They describe their findings - and their stroke of luck - in a study [link above], shedding light on a mechanism that made roughly two-thirds of Earth’s crust…”
    --
    #Seabed2030 #OceanMapping #Hydrospatial #remotesensing #seafloor #seafloorspreading #oceanic #crust #geology #structuralgeology #IndianOcean #earthquake #midoceanridge #instrumentation #marine #seabed #hydrography #model #modeling #mapping #GIS #spatial #tectonicplates #magma #fortuitous #survey #seismogeodetic #monitoring #submarine #rifting #observation #volcanism #seismicity #dyke #fault #faulting #midoceanridge #MOR

  28. Anatomy Of A Seafloor Spreading Event Captured By In Situ Seismogeodesy
    --
    doi.org/10.1038/s41586-026-107 <-- shared paper
    --
    smithsonianmag.com/smart-news/ <-- shared technical media article
    --
    H/T @Seabed 2030
    “🔍 For the first time, scientists have observed seafloor spreading in real time.
    Seafloor spreading is the process by which new oceanic crust is formed at mid-ocean ridges - a geological process that has shaped entire ocean basins over millions of years.
    During a research expedition in the Indian Ocean, scientists had just deployed a suite of instruments when a series of earthquakes triggered a seafloor spreading event, allowing them to observe the process as it unfolded.
    The findings offer rare new insights into how new oceanic crust forms and how the seafloor continues to evolve…”
    --
    “Earth’s outermost layer - the crust - is constantly renewing itself. It’s broken into giant chunks called tectonic plates that pull apart, push against or slide past one another, creating grand geologic features.
    Underwater mountain ranges, or mid-ocean ridges, for instance, generally take shape where two tectonic plates are moving away from each other. Magma can then bubble up in between, solidifying and turning into new oceanic crust as part of a process called seafloor spreading. Although the phenomenon has created entire ocean basins, it remains quite mysterious because it happens so deep in the water.
    Now, for the first time, scientists have observed this dynamic activity happening in real time. They describe their findings - and their stroke of luck - in a study [link above], shedding light on a mechanism that made roughly two-thirds of Earth’s crust…”
    --
    #Seabed2030 #OceanMapping #Hydrospatial #remotesensing #seafloor #seafloorspreading #oceanic #crust #geology #structuralgeology #IndianOcean #earthquake #midoceanridge #instrumentation #marine #seabed #hydrography #model #modeling #mapping #GIS #spatial #tectonicplates #magma #fortuitous #survey #seismogeodetic #monitoring #submarine #rifting #observation #volcanism #seismicity #dyke #fault #faulting #midoceanridge #MOR

  29. Anatomy Of A Seafloor Spreading Event Captured By In Situ Seismogeodesy
    --
    doi.org/10.1038/s41586-026-107 <-- shared paper
    --
    smithsonianmag.com/smart-news/ <-- shared technical media article
    --
    H/T @Seabed 2030
    “🔍 For the first time, scientists have observed seafloor spreading in real time.
    Seafloor spreading is the process by which new oceanic crust is formed at mid-ocean ridges - a geological process that has shaped entire ocean basins over millions of years.
    During a research expedition in the Indian Ocean, scientists had just deployed a suite of instruments when a series of earthquakes triggered a seafloor spreading event, allowing them to observe the process as it unfolded.
    The findings offer rare new insights into how new oceanic crust forms and how the seafloor continues to evolve…”
    --
    “Earth’s outermost layer - the crust - is constantly renewing itself. It’s broken into giant chunks called tectonic plates that pull apart, push against or slide past one another, creating grand geologic features.
    Underwater mountain ranges, or mid-ocean ridges, for instance, generally take shape where two tectonic plates are moving away from each other. Magma can then bubble up in between, solidifying and turning into new oceanic crust as part of a process called seafloor spreading. Although the phenomenon has created entire ocean basins, it remains quite mysterious because it happens so deep in the water.
    Now, for the first time, scientists have observed this dynamic activity happening in real time. They describe their findings - and their stroke of luck - in a study [link above], shedding light on a mechanism that made roughly two-thirds of Earth’s crust…”
    --

  30. Ice Giant or Magma Ocean World?

    Uranus and Neptune–known as our system’s ice giants–are our least explored planets. Both have received exactly one flyby, from the Voyager 2 spacecraft. The data from those flybys remain our primary source of knowledge about each planet. The traditional model for each planet’s interior (dating back to before the flybys) consists of three layers: a rocky core; an icy mantle made up of water, ammonia, and methane; and a hydrogen/helium-rich atmosphere. That structure is one way to match the limited measurements we have from these planets, but, as today’s preprint study points out, it’s not the only way.

    The authors suggest an alternative structure, in which a hydrogen-rich atmosphere overlays a supercritical magma ocean capable of dissolving hydrogen into heavier, metallic elements. Their suggestion is motivated by several factors. First, objects in the outer solar system–including Kuiper Belt objects–have less icy material than originally assumed, which suggests that Uranus and Neptune’s progenitors wouldn’t have been so ice-rich, either. Second, our understanding of how “rocky” materials respond at the temperatures and pressures found in these planet interiors has evolved. In particular, silicate, hydrogen, and iron are actually miscible at these conditions. That means that discrete sub-layers separated by material type are not as likely.

    Using the magma ocean model, the team found compositions for both Uranus and Neptune that conformed well to our limited data about their gravitational and magnetic field properties. Time–and more data–will tell as to which interior model best describes these enigmatic giants. (Image credit: NASA; research credit: E. Young et al. (preprint); via Gizmodo)

    #fluidDynamics #geophysics #magma #miscibility #numericalSimulation #physics #planetaryScience #science #supercriticalFluids
  31. Ice Giant or Magma Ocean World?

    Uranus and Neptune–known as our system’s ice giants–are our least explored planets. Both have received exactly one flyby, from the Voyager 2 spacecraft. The data from those flybys remain our primary source of knowledge about each planet. The traditional model for each planet’s interior (dating back to before the flybys) consists of three layers: a rocky core; an icy mantle made up of water, ammonia, and methane; and a hydrogen/helium-rich atmosphere. That structure is one way to match the limited measurements we have from these planets, but, as today’s preprint study points out, it’s not the only way.

    The authors suggest an alternative structure, in which a hydrogen-rich atmosphere overlays a supercritical magma ocean capable of dissolving hydrogen into heavier, metallic elements. Their suggestion is motivated by several factors. First, objects in the outer solar system–including Kuiper Belt objects–have less icy material than originally assumed, which suggests that Uranus and Neptune’s progenitors wouldn’t have been so ice-rich, either. Second, our understanding of how “rocky” materials respond at the temperatures and pressures found in these planet interiors has evolved. In particular, silicate, hydrogen, and iron are actually miscible at these conditions. That means that discrete sub-layers separated by material type are not as likely.

    Using the magma ocean model, the team found compositions for both Uranus and Neptune that conformed well to our limited data about their gravitational and magnetic field properties. Time–and more data–will tell as to which interior model best describes these enigmatic giants. (Image credit: NASA; research credit: E. Young et al. (preprint); via Gizmodo)

    #fluidDynamics #geophysics #magma #miscibility #numericalSimulation #physics #planetaryScience #science #supercriticalFluids
  32. Ice Giant or Magma Ocean World?

    Uranus and Neptune–known as our system’s ice giants–are our least explored planets. Both have received exactly one flyby, from the Voyager 2 spacecraft. The data from those flybys remain our primary source of knowledge about each planet. The traditional model for each planet’s interior (dating back to before the flybys) consists of three layers: a rocky core; an icy mantle made up of water, ammonia, and methane; and a hydrogen/helium-rich atmosphere. That structure is one way to match the limited measurements we have from these planets, but, as today’s preprint study points out, it’s not the only way.

    The authors suggest an alternative structure, in which a hydrogen-rich atmosphere overlays a supercritical magma ocean capable of dissolving hydrogen into heavier, metallic elements. Their suggestion is motivated by several factors. First, objects in the outer solar system–including Kuiper Belt objects–have less icy material than originally assumed, which suggests that Uranus and Neptune’s progenitors wouldn’t have been so ice-rich, either. Second, our understanding of how “rocky” materials respond at the temperatures and pressures found in these planet interiors has evolved. In particular, silicate, hydrogen, and iron are actually miscible at these conditions. That means that discrete sub-layers separated by material type are not as likely.

    Using the magma ocean model, the team found compositions for both Uranus and Neptune that conformed well to our limited data about their gravitational and magnetic field properties. Time–and more data–will tell as to which interior model best describes these enigmatic giants. (Image credit: NASA; research credit: E. Young et al. (preprint); via Gizmodo)

    #fluidDynamics #geophysics #magma #miscibility #numericalSimulation #physics #planetaryScience #science #supercriticalFluids
  33. Ice Giant or Magma Ocean World?

    Uranus and Neptune–known as our system’s ice giants–are our least explored planets. Both have received exactly one flyby, from the Voyager 2 spacecraft. The data from those flybys remain our primary source of knowledge about each planet. The traditional model for each planet’s interior (dating back to before the flybys) consists of three layers: a rocky core; an icy mantle made up of water, ammonia, and methane; and a hydrogen/helium-rich atmosphere. That structure is one way to match the limited measurements we have from these planets, but, as today’s preprint study points out, it’s not the only way.

    The authors suggest an alternative structure, in which a hydrogen-rich atmosphere overlays a supercritical magma ocean capable of dissolving hydrogen into heavier, metallic elements. Their suggestion is motivated by several factors. First, objects in the outer solar system–including Kuiper Belt objects–have less icy material than originally assumed, which suggests that Uranus and Neptune’s progenitors wouldn’t have been so ice-rich, either. Second, our understanding of how “rocky” materials respond at the temperatures and pressures found in these planet interiors has evolved. In particular, silicate, hydrogen, and iron are actually miscible at these conditions. That means that discrete sub-layers separated by material type are not as likely.

    Using the magma ocean model, the team found compositions for both Uranus and Neptune that conformed well to our limited data about their gravitational and magnetic field properties. Time–and more data–will tell as to which interior model best describes these enigmatic giants. (Image credit: NASA; research credit: E. Young et al. (preprint); via Gizmodo)

    #fluidDynamics #geophysics #magma #miscibility #numericalSimulation #physics #planetaryScience #science #supercriticalFluids
  34. Ice Giant or Magma Ocean World?

    Uranus and Neptune–known as our system’s ice giants–are our least explored planets. Both have received exactly one flyby, from the Voyager 2 spacecraft. The data from those flybys remain our primary source of knowledge about each planet. The traditional model for each planet’s interior (dating back to before the flybys) consists of three layers: a rocky core; an icy mantle made up of water, ammonia, and methane; and a hydrogen/helium-rich atmosphere. That structure is one way to match the limited measurements we have from these planets, but, as today’s preprint study points out, it’s not the only way.

    The authors suggest an alternative structure, in which a hydrogen-rich atmosphere overlays a supercritical magma ocean capable of dissolving hydrogen into heavier, metallic elements. Their suggestion is motivated by several factors. First, objects in the outer solar system–including Kuiper Belt objects–have less icy material than originally assumed, which suggests that Uranus and Neptune’s progenitors wouldn’t have been so ice-rich, either. Second, our understanding of how “rocky” materials respond at the temperatures and pressures found in these planet interiors has evolved. In particular, silicate, hydrogen, and iron are actually miscible at these conditions. That means that discrete sub-layers separated by material type are not as likely.

    Using the magma ocean model, the team found compositions for both Uranus and Neptune that conformed well to our limited data about their gravitational and magnetic field properties. Time–and more data–will tell as to which interior model best describes these enigmatic giants. (Image credit: NASA; research credit: E. Young et al. (preprint); via Gizmodo)

    #fluidDynamics #geophysics #magma #miscibility #numericalSimulation #physics #planetaryScience #science #supercriticalFluids
  35. The Genesis GV60 Magma Is $9,000 Pricier Than Its Hyundai Sibling

    The 2027 Genesis GV60 Magma starts at $71,495 (including destination fees). It’s initially available at dealers in California, New…
    #EuropeSays #Korea #KR #HyundaiMotor #audisport #B2C #bev #bmwm #csuv #fastcharging #Genesis #genesisgv60 #GenesisGV60Magma #highperformance #Hyundai #HyundaiMotorGroup #Ioniq5N #Kia #luxury #magma #mercedesamg #Opinion #Pricing #sporty #SUV #SUV/Crossover
    europesays.com/korea/104005/

  36. Deep beneath Mars's volcanoes, InSight found a hidden network of magma highways

    Follow @1ban_news for daily coverage.

    1ban.news/mars-magma-rivers-in

    #1ban #mars #magma #rivers #insight #space

  37. I been busy but hey, I'm alive! Here's some random Jojo drawing I did for practice.

    #jojo #fanart #magma #sketch #digitalArt #art #artistsonmastodon #mastoart

  38. I been busy but hey, I'm alive! Here's some random Jojo drawing I did for practice.

    #jojo #fanart #magma #sketch #digitalArt #art #artistsonmastodon #mastoart

  39. I been busy but hey, I'm alive! Here's some random Jojo drawing I did for practice.

    #jojo #fanart #magma #sketch #digitalArt #art #artistsonmastodon #mastoart

  40. WHAT’S ON THE SHELF, JULY 22ND – INDEPENDENT PUBLISHERS
    What’s on the Shelf is built from distributor order forms and shipping date information, giving fans a heads-up on what may be landing at their local...
    comiccrusaders.com/comics/comi
    #07222026 #comic books #comics #Ignition Press #independent #Indie #Indie Comics #kodansha #mad cave #magma #Manga #ncbd #New Comic Book Day #New Comics #oni #viz #what's on the shelf

  41. WHAT’S ON THE SHELF, JULY 22ND – INDEPENDENT PUBLISHERS
    What’s on the Shelf is built from distributor order forms and shipping date information, giving fans a heads-up on what may be landing at their local...
    comiccrusaders.com/comics/comi
    #07222026 #comic books #comics #Ignition Press #independent #Indie #Indie Comics #kodansha #mad cave #magma #Manga #ncbd #New Comic Book Day #New Comics #oni #viz #what's on the shelf

  42. Last classes of the week were in town, and since it's become a bit of a tradition, here is this week's vinyl purchase.

    The debut Magma album, also known as Kobaïa, which I've never owned a physical copy of. Might sound a bit more like early 70s modern European electric jazz than some of their later offerings, but I happen to like early 70s modern European electric jazz a lot, so no complaints from me. Excellent exacting and dynamic pressing. Ïma sürï Dondaï, as they say.

    #vinyl #magma #zeuhl

  43. Last classes of the week were in town, and since it's become a bit of a tradition, here is this week's vinyl purchase.

    The debut Magma album, also known as Kobaïa, which I've never owned a physical copy of. Might sound a bit more like early 70s modern European electric jazz than some of their later offerings, but I happen to like early 70s modern European electric jazz a lot, so no complaints from me. Excellent exacting and dynamic pressing. Ïma sürï Dondaï, as they say.

    #vinyl #magma #zeuhl

  44. Last classes of the week were in town, and since it's become a bit of a tradition, here is this week's vinyl purchase.

    The debut Magma album, also known as Kobaïa, which I've never owned a physical copy of. Might sound a bit more like early 70s modern European electric jazz than some of their later offerings, but I happen to like early 70s modern European electric jazz a lot, so no complaints from me. Excellent exacting and dynamic pressing. Ïma sürï Dondaï, as they say.

    #vinyl #magma #zeuhl

  45. Last classes of the week were in town, and since it's become a bit of a tradition, here is this week's vinyl purchase.

    The debut Magma album, also known as Kobaïa, which I've never owned a physical copy of. Might sound a bit more like early 70s modern European electric jazz than some of their later offerings, but I happen to like early 70s modern European electric jazz a lot, so no complaints from me. Excellent exacting and dynamic pressing. Ïma sürï Dondaï, as they say.

    #vinyl #magma #zeuhl