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#geophysics — Public Fediverse posts

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

  1. 🚨Job Alert ‼️🚨 Actually, three (3) openings:
    1) Adjunct Prof with industry experience in economic #geology and ore systems science
    2) Lecturer, Sr Lecturer, or Assoc Prof, hydrogeology, geometallurgy, etc
    3) Computational #geophysics
    wits.ac.za/vacancies/
    Univ Witwatersrand, S Africa
    🧪⚒️

  2. 🚨Job Alert ‼️🚨 Actually, three (3) openings:
    1) Adjunct Prof with industry experience in economic #geology and ore systems science
    2) Lecturer, Sr Lecturer, or Assoc Prof, hydrogeology, geometallurgy, etc
    3) Computational #geophysics
    wits.ac.za/vacancies/
    Univ Witwatersrand, S Africa
    🧪⚒️

  3. Múlajökull

    Iceland’s Múlajökull glacier is prone to sudden surges, where rapid ice flow is interspersed between periods of quiescence or retreat. The isolated nature of the glacier and its marshy surroundings make approaching on foot almost impossible, but photographer Dani Guindo captured gorgeous aerial images of the glacier’s many rivulets ribboning about the landscape it’s carved. (Image credit: D. Guindo; via Colossal)

    #fluidDynamics #geophysics #glacier #instability #meander #physics #rivers #science
  4. Múlajökull

    Iceland’s Múlajökull glacier is prone to sudden surges, where rapid ice flow is interspersed between periods of quiescence or retreat. The isolated nature of the glacier and its marshy surroundings make approaching on foot almost impossible, but photographer Dani Guindo captured gorgeous aerial images of the glacier’s many rivulets ribboning about the landscape it’s carved. (Image credit: D. Guindo; via Colossal)

    #fluidDynamics #geophysics #glacier #instability #meander #physics #rivers #science
  5. Múlajökull

    Iceland’s Múlajökull glacier is prone to sudden surges, where rapid ice flow is interspersed between periods of quiescence or retreat. The isolated nature of the glacier and its marshy surroundings make approaching on foot almost impossible, but photographer Dani Guindo captured gorgeous aerial images of the glacier’s many rivulets ribboning about the landscape it’s carved. (Image credit: D. Guindo; via Colossal)

    #fluidDynamics #geophysics #glacier #instability #meander #physics #rivers #science
  6. Múlajökull

    Iceland’s Múlajökull glacier is prone to sudden surges, where rapid ice flow is interspersed between periods of quiescence or retreat. The isolated nature of the glacier and its marshy surroundings make approaching on foot almost impossible, but photographer Dani Guindo captured gorgeous aerial images of the glacier’s many rivulets ribboning about the landscape it’s carved. (Image credit: D. Guindo; via Colossal)

    #fluidDynamics #geophysics #glacier #instability #meander #physics #rivers #science
  7. Múlajökull

    Iceland’s Múlajökull glacier is prone to sudden surges, where rapid ice flow is interspersed between periods of quiescence or retreat. The isolated nature of the glacier and its marshy surroundings make approaching on foot almost impossible, but photographer Dani Guindo captured gorgeous aerial images of the glacier’s many rivulets ribboning about the landscape it’s carved. (Image credit: D. Guindo; via Colossal)

    #fluidDynamics #geophysics #glacier #instability #meander #physics #rivers #science
  8. Convection Inside the Mantle

    Most of what we know about Earth’s interior comes from observing how seismic waves–mostly from earthquakes–bounce around. As our observations have gotten better–more seisometers, better imaging techniques–scientists have identified two large anomalies sitting near the bottom of the mantle. Known as large low-velocity provinces, or LLVPs, these zones take up continent-sized areas beneath parts of Africa and the Pacific.

    Seismic waves show lower speeds in large, continent-sized zones that sit beneath Africa and the Pacific. These large low-velocity provinces (LLVPs) are outlined in red.

    The LLVPs are hot, which would normally make them buoyant, but their stationary nature suggests they are made up of extremely dense material. Narrow plumes of hot material make their way up from the LLVPs to form volcanic hotspots like those that made the Hawaiian and Galapagos Islands. Balancing that upward convection is the downward convection of former tectonic material carried into the mantle at subduction zones.

    What the LLVPs are made of remains an active research question. One suggestion is that they contain remnants of Theia, the planet thought to have impacted the proto-Earth to form our Moon. (Image credits: E. Garnero and C. Richardson; see also Physics Today)

    Illustration showing convection in the Earth’s inner mantle. Former tectonic material subducts downward in dark blue zones. The large low-velocity provinces (LLVPs) are shown in orange. Hot-spot volcanic activity is seen at the surface (black triangles) above narrow plumes that lift material from the LLVPs toward the surface. #buoyancy #convection #fluidDynamics #geophysics #mantleConvection #physics #science #seismicWaves
  9. Convection Inside the Mantle

    Most of what we know about Earth’s interior comes from observing how seismic waves–mostly from earthquakes–bounce around. As our observations have gotten better–more seisometers, better imaging techniques–scientists have identified two large anomalies sitting near the bottom of the mantle. Known as large low-velocity provinces, or LLVPs, these zones take up continent-sized areas beneath parts of Africa and the Pacific.

    Seismic waves show lower speeds in large, continent-sized zones that sit beneath Africa and the Pacific. These large low-velocity provinces (LLVPs) are outlined in red.

    The LLVPs are hot, which would normally make them buoyant, but their stationary nature suggests they are made up of extremely dense material. Narrow plumes of hot material make their way up from the LLVPs to form volcanic hotspots like those that made the Hawaiian and Galapagos Islands. Balancing that upward convection is the downward convection of former tectonic material carried into the mantle at subduction zones.

    What the LLVPs are made of remains an active research question. One suggestion is that they contain remnants of Theia, the planet thought to have impacted the proto-Earth to form our Moon. (Image credits: E. Garnero and C. Richardson; see also Physics Today)

    Illustration showing convection in the Earth’s inner mantle. Former tectonic material subducts downward in dark blue zones. The large low-velocity provinces (LLVPs) are shown in orange. Hot-spot volcanic activity is seen at the surface (black triangles) above narrow plumes that lift material from the LLVPs toward the surface. #buoyancy #convection #fluidDynamics #geophysics #mantleConvection #physics #science #seismicWaves
  10. European summer drying largely driven by atmospheric circulation changes since the 1980s

    Bevacqua, E. et al. Direct and lagged climate change effects intensified the 2022 European drought. Nat. Geosci. doi.org/10.1038/s41561-024-015
    #Europe #EU #Atmosphericdynamics #Attribution #earthsciences #EarthSystemSciences #general #Geochemistry #geology #Geophysics/Geodesy #Hydrology
    europesays.com/europe/100574/

  11. Geophysics is the scientific study of the Earth and its surrounding space environment using the quantitative methods of physics.
    #Geophysics #EarthScience #sflorg
    sflorg.com/2026/07/cat07202601

  12. Geophysics is the scientific study of the Earth and its surrounding space environment using the quantitative methods of physics.
    #Geophysics #EarthScience #sflorg
    sflorg.com/2026/07/cat07202601

  13. Geophysics is the scientific study of the Earth and its surrounding space environment using the quantitative methods of physics.
    #Geophysics #EarthScience #sflorg
    sflorg.com/2026/07/cat07202601

  14. Geophysics is the scientific study of the Earth and its surrounding space environment using the quantitative methods of physics.
    #Geophysics #EarthScience #sflorg
    sflorg.com/2026/07/cat07202601

  15. Geophysics is the scientific study of the Earth and its surrounding space environment using the quantitative methods of physics.
    #Geophysics #EarthScience #sflorg
    sflorg.com/2026/07/cat07202601

  16. February 24, 2026 Kyoto University scientists propose a theoretical link between solar flares and earthquakes: ionosphere charge shifts could create electrostatic pressure inside fractured fault zones 🌌⚡️🌍. The model doesn’t predict quakes—explores a possible mechanism. sciencedaily.com/releases/2026 #SpaceWeather #Earthquakes #Geophysics

  17. February 24, 2026 Kyoto University scientists propose a theoretical link between solar flares and earthquakes: ionosphere charge shifts could create electrostatic pressure inside fractured fault zones 🌌⚡️🌍. The model doesn’t predict quakes—explores a possible mechanism. sciencedaily.com/releases/2026 #SpaceWeather #Earthquakes #Geophysics

  18. Mirabilite Mounds at Great Salt Lake

    In cold weather, a new geological feature has shown up at Utah’s Great Salt Lake in the last decade. These salty mirabilite mounds form terraced crystals that resemble Yellowstone’s Mammoth Hot Springs.

    Diagram showing how a salt-laden spring pushing upward through the mirabilite layer can then form mounds at the surface when the dissolved mirabilite recrystallizes after the water evaporates.

    Mirabilite is hydrated sodium sulfate (as opposed to the sodium chloride of table salt). The structures form when upwelling spring water partially dissolves the layer of mirabilite found beneath the lake bed. That sulfate-laden water rises to the surface, where it freezes into the crystals seen here.

    A timelapse showing the formation of mirabilite mounds.

    When temperatures rise above freezing, the water in the mirabilite evaporates, leaving behind white, powdery thenardite. (Video credit: Great Salt Lake Institute; image credit: Utah Geological Survey)

    #crystalGrowth #dissolution #evaporation #fluidDynamics #freezing #geophysics #physics #science
  19. Mirabilite Mounds at Great Salt Lake

    In cold weather, a new geological feature has shown up at Utah’s Great Salt Lake in the last decade. These salty mirabilite mounds form terraced crystals that resemble Yellowstone’s Mammoth Hot Springs.

    Diagram showing how a salt-laden spring pushing upward through the mirabilite layer can then form mounds at the surface when the dissolved mirabilite recrystallizes after the water evaporates.

    Mirabilite is hydrated sodium sulfate (as opposed to the sodium chloride of table salt). The structures form when upwelling spring water partially dissolves the layer of mirabilite found beneath the lake bed. That sulfate-laden water rises to the surface, where it freezes into the crystals seen here.

    A timelapse showing the formation of mirabilite mounds.

    When temperatures rise above freezing, the water in the mirabilite evaporates, leaving behind white, powdery thenardite. (Video credit: Great Salt Lake Institute; image credit: Utah Geological Survey)

    #crystalGrowth #dissolution #evaporation #fluidDynamics #freezing #geophysics #physics #science
  20. Mirabilite Mounds at Great Salt Lake

    In cold weather, a new geological feature has shown up at Utah’s Great Salt Lake in the last decade. These salty mirabilite mounds form terraced crystals that resemble Yellowstone’s Mammoth Hot Springs.

    Diagram showing how a salt-laden spring pushing upward through the mirabilite layer can then form mounds at the surface when the dissolved mirabilite recrystallizes after the water evaporates.

    Mirabilite is hydrated sodium sulfate (as opposed to the sodium chloride of table salt). The structures form when upwelling spring water partially dissolves the layer of mirabilite found beneath the lake bed. That sulfate-laden water rises to the surface, where it freezes into the crystals seen here.

    A timelapse showing the formation of mirabilite mounds.

    When temperatures rise above freezing, the water in the mirabilite evaporates, leaving behind white, powdery thenardite. (Video credit: Great Salt Lake Institute; image credit: Utah Geological Survey)

    #crystalGrowth #dissolution #evaporation #fluidDynamics #freezing #geophysics #physics #science
  21. Mirabilite Mounds at Great Salt Lake

    In cold weather, a new geological feature has shown up at Utah’s Great Salt Lake in the last decade. These salty mirabilite mounds form terraced crystals that resemble Yellowstone’s Mammoth Hot Springs.

    Diagram showing how a salt-laden spring pushing upward through the mirabilite layer can then form mounds at the surface when the dissolved mirabilite recrystallizes after the water evaporates.

    Mirabilite is hydrated sodium sulfate (as opposed to the sodium chloride of table salt). The structures form when upwelling spring water partially dissolves the layer of mirabilite found beneath the lake bed. That sulfate-laden water rises to the surface, where it freezes into the crystals seen here.

    A timelapse showing the formation of mirabilite mounds.

    When temperatures rise above freezing, the water in the mirabilite evaporates, leaving behind white, powdery thenardite. (Video credit: Great Salt Lake Institute; image credit: Utah Geological Survey)

    #crystalGrowth #dissolution #evaporation #fluidDynamics #freezing #geophysics #physics #science
  22. Mirabilite Mounds at Great Salt Lake

    In cold weather, a new geological feature has shown up at Utah’s Great Salt Lake in the last decade. These salty mirabilite mounds form terraced crystals that resemble Yellowstone’s Mammoth Hot Springs.

    Diagram showing how a salt-laden spring pushing upward through the mirabilite layer can then form mounds at the surface when the dissolved mirabilite recrystallizes after the water evaporates.

    Mirabilite is hydrated sodium sulfate (as opposed to the sodium chloride of table salt). The structures form when upwelling spring water partially dissolves the layer of mirabilite found beneath the lake bed. That sulfate-laden water rises to the surface, where it freezes into the crystals seen here.

    A timelapse showing the formation of mirabilite mounds.

    When temperatures rise above freezing, the water in the mirabilite evaporates, leaving behind white, powdery thenardite. (Video credit: Great Salt Lake Institute; image credit: Utah Geological Survey)

    #crystalGrowth #dissolution #evaporation #fluidDynamics #freezing #geophysics #physics #science
  23. In a first, scientists observe the formation of the oceanic crust

    Researchers at the French National Center of Scientific Research have become the first to observe the formation of…
    #NewsBeep #News #Environment #AU #Australia #faults #FrenchNationalCenterofScientificResearch #Geophysics #Hydro-AcousticsandGeodesynearAmsterdamIsland #lava #oceanfloor #quantumevents #Ridge #SaintPaul-Amsterdamvolcanicplateau #Science #seafloor #SoutheastIndianRidge
    newsbeep.com/au/792295/

  24. In a first, scientists observe the formation of the oceanic crust

    Researchers at the French National Center of Scientific Research have become the first to observe the formation of…
    #NewsBeep #News #Environment #AU #Australia #faults #FrenchNationalCenterofScientificResearch #Geophysics #Hydro-AcousticsandGeodesynearAmsterdamIsland #lava #oceanfloor #quantumevents #Ridge #SaintPaul-Amsterdamvolcanicplateau #Science #seafloor #SoutheastIndianRidge
    newsbeep.com/au/792295/

  25. In a first, scientists observe the formation of the oceanic crust

    Researchers at the French National Center of Scientific Research have become the first to observe the formatio…
    #NewsBeep #News #Environment #environment #faults #FrenchNationalCenterofScientificResearch #Geophysics #Hydro-AcousticsandGeodesynearAmsterdamIsland #lava #oceanfloor #quantumevents #ridge #SaintPaul-Amsterdamvolcanicplateau #Science #seafloor #SoutheastIndianRidge #UK #UnitedKingdom
    newsbeep.com/uk/684951/

  26. Anatomy of a seafloor spreading event captured by in situ seismogeodesy

    Macdonald, K. C. Mid-ocean ridges: fine scale tectonic, volcanic and hydrothermal processes within the plate boundary zone. Annu.…
    #NewsBeep #News #US #USA #UnitedStates #UnitedStatesOfAmerica #Science #Geodynamics #Geophysics #HumanitiesandSocialSciences #multidisciplinary #Tectonics
    newsbeep.com/us/751655/

  27. Anatomy of a seafloor spreading event captured by in situ seismogeodesy

    Macdonald, K. C. Mid-ocean ridges: fine scale tectonic, volcanic and hydrothermal processes within the plate boundary zone. Annu.…
    #NewsBeep #News #US #USA #UnitedStates #UnitedStatesOfAmerica #Science #Geodynamics #Geophysics #HumanitiesandSocialSciences #multidisciplinary #Tectonics
    newsbeep.com/us/751655/

  28. The Disappearing Great Salt Lake

    Since 1989, Utah’s Great Salt Lake has lost some 70% of its surface area. The exposed lakebed left behind is a source of toxic dust that gets lifted into the air. Researchers are trying to understand what water sources exist beneath the lake and whether they might save the saline lake and its ecosystem from disappearing entirely.

    A recent study pinpoints underground water by measuring the electrical resistance between electrodes placed meters apart in the ground (photo above). Because salty water is more electrically conductive than fresh water, the researchers can distinguish between them. So far, they’ve found quite a lot of fresh water, sometimes only a couple meters below the surface. But those patches are often quite close to saline water, too.

    The group also described to Eos that they found mounds of invasive reeds lying atop concentrations of fresh water. The invasive species seems to be sucking up water that would otherwise feed back into the lake or support native plants that provide habitat to native birds. (Image credit: M. Thorne; research credit: M. Jacketta et al.; via Eos)

    #fluidDynamics #geophysics #physics #porousFlow #salineLakes #science
  29. The Disappearing Great Salt Lake

    Since 1989, Utah’s Great Salt Lake has lost some 70% of its surface area. The exposed lakebed left behind is a source of toxic dust that gets lifted into the air. Researchers are trying to understand what water sources exist beneath the lake and whether they might save the saline lake and its ecosystem from disappearing entirely.

    A recent study pinpoints underground water by measuring the electrical resistance between electrodes placed meters apart in the ground (photo above). Because salty water is more electrically conductive than fresh water, the researchers can distinguish between them. So far, they’ve found quite a lot of fresh water, sometimes only a couple meters below the surface. But those patches are often quite close to saline water, too.

    The group also described to Eos that they found mounds of invasive reeds lying atop concentrations of fresh water. The invasive species seems to be sucking up water that would otherwise feed back into the lake or support native plants that provide habitat to native birds. (Image credit: M. Thorne; research credit: M. Jacketta et al.; via Eos)

    #fluidDynamics #geophysics #physics #porousFlow #salineLakes #science
  30. The Disappearing Great Salt Lake

    Since 1989, Utah’s Great Salt Lake has lost some 70% of its surface area. The exposed lakebed left behind is a source of toxic dust that gets lifted into the air. Researchers are trying to understand what water sources exist beneath the lake and whether they might save the saline lake and its ecosystem from disappearing entirely.

    A recent study pinpoints underground water by measuring the electrical resistance between electrodes placed meters apart in the ground (photo above). Because salty water is more electrically conductive than fresh water, the researchers can distinguish between them. So far, they’ve found quite a lot of fresh water, sometimes only a couple meters below the surface. But those patches are often quite close to saline water, too.

    The group also described to Eos that they found mounds of invasive reeds lying atop concentrations of fresh water. The invasive species seems to be sucking up water that would otherwise feed back into the lake or support native plants that provide habitat to native birds. (Image credit: M. Thorne; research credit: M. Jacketta et al.; via Eos)

    #fluidDynamics #geophysics #physics #porousFlow #salineLakes #science
  31. The Disappearing Great Salt Lake

    Since 1989, Utah’s Great Salt Lake has lost some 70% of its surface area. The exposed lakebed left behind is a source of toxic dust that gets lifted into the air. Researchers are trying to understand what water sources exist beneath the lake and whether they might save the saline lake and its ecosystem from disappearing entirely.

    A recent study pinpoints underground water by measuring the electrical resistance between electrodes placed meters apart in the ground (photo above). Because salty water is more electrically conductive than fresh water, the researchers can distinguish between them. So far, they’ve found quite a lot of fresh water, sometimes only a couple meters below the surface. But those patches are often quite close to saline water, too.

    The group also described to Eos that they found mounds of invasive reeds lying atop concentrations of fresh water. The invasive species seems to be sucking up water that would otherwise feed back into the lake or support native plants that provide habitat to native birds. (Image credit: M. Thorne; research credit: M. Jacketta et al.; via Eos)

    #fluidDynamics #geophysics #physics #porousFlow #salineLakes #science
  32. The Disappearing Great Salt Lake

    Since 1989, Utah’s Great Salt Lake has lost some 70% of its surface area. The exposed lakebed left behind is a source of toxic dust that gets lifted into the air. Researchers are trying to understand what water sources exist beneath the lake and whether they might save the saline lake and its ecosystem from disappearing entirely.

    A recent study pinpoints underground water by measuring the electrical resistance between electrodes placed meters apart in the ground (photo above). Because salty water is more electrically conductive than fresh water, the researchers can distinguish between them. So far, they’ve found quite a lot of fresh water, sometimes only a couple meters below the surface. But those patches are often quite close to saline water, too.

    The group also described to Eos that they found mounds of invasive reeds lying atop concentrations of fresh water. The invasive species seems to be sucking up water that would otherwise feed back into the lake or support native plants that provide habitat to native birds. (Image credit: M. Thorne; research credit: M. Jacketta et al.; via Eos)

    #fluidDynamics #geophysics #physics #porousFlow #salineLakes #science
  33. Researchers have identified a practical upper bound for material viscosity, estimated at 10³⁰±² Pa s, beyond which substances function as essentially rigid bodies over finite timescales.
    #Geophysics #MineralPhysics #FluidDynamics #MaterialsScience #sflorg
    sflorg.com/2026/07/phy07062601

  34. Researchers have identified a practical upper bound for material viscosity, estimated at 10³⁰±² Pa s, beyond which substances function as essentially rigid bodies over finite timescales.
    #Geophysics #MineralPhysics #FluidDynamics #MaterialsScience #sflorg
    sflorg.com/2026/07/phy07062601

  35. Researchers have identified a practical upper bound for material viscosity, estimated at 10³⁰±² Pa s, beyond which substances function as essentially rigid bodies over finite timescales.
    #Geophysics #MineralPhysics #FluidDynamics #MaterialsScience #sflorg
    sflorg.com/2026/07/phy07062601

  36. Researchers have identified a practical upper bound for material viscosity, estimated at 10³⁰±² Pa s, beyond which substances function as essentially rigid bodies over finite timescales.
    #Geophysics #MineralPhysics #FluidDynamics #MaterialsScience #sflorg
    sflorg.com/2026/07/phy07062601

  37. Researchers have identified a practical upper bound for material viscosity, estimated at 10³⁰±² Pa s, beyond which substances function as essentially rigid bodies over finite timescales.
    #Geophysics #MineralPhysics #FluidDynamics #MaterialsScience #sflorg
    sflorg.com/2026/07/phy07062601

  38. ✨#42 of #85ThingsAboutDIAS

    The Irish National Seismic Network

    The Geophysics Section of DIAS operates the Irish National Seismic Network (INSN). Established in 1980, the network monitors seismic activity across Ireland - through a series of stations. Seismic data is transmitted in real time to the INSN data centre at 5 Merrion Square and shared internationally.

    #DIASdiscovers #INSN #geophysics

  39. ✨#42 of #85ThingsAboutDIAS

    The Irish National Seismic Network

    The Geophysics Section of DIAS operates the Irish National Seismic Network (INSN). Established in 1980, the network monitors seismic activity across Ireland - through a series of stations. Seismic data is transmitted in real time to the INSN data centre at 5 Merrion Square and shared internationally.

    #DIASdiscovers #INSN #geophysics

  40. ✨#42 of #85ThingsAboutDIAS

    The Irish National Seismic Network

    The Geophysics Section of DIAS operates the Irish National Seismic Network (INSN). Established in 1980, the network monitors seismic activity across Ireland - through a series of stations. Seismic data is transmitted in real time to the INSN data centre at 5 Merrion Square and shared internationally.

    #DIASdiscovers #INSN #geophysics

  41. ✨#42 of #85ThingsAboutDIAS

    The Irish National Seismic Network

    The Geophysics Section of DIAS operates the Irish National Seismic Network (INSN). Established in 1980, the network monitors seismic activity across Ireland - through a series of stations. Seismic data is transmitted in real time to the INSN data centre at 5 Merrion Square and shared internationally.

    #DIASdiscovers #INSN #geophysics

  42. ✨#42 of #85ThingsAboutDIAS

    The Irish National Seismic Network

    The Geophysics Section of DIAS operates the Irish National Seismic Network (INSN). Established in 1980, the network monitors seismic activity across Ireland - through a series of stations. Seismic data is transmitted in real time to the INSN data centre at 5 Merrion Square and shared internationally.

    #DIASdiscovers #INSN #geophysics

  43. 💁🏻‍♀️ ICYMI: 🌋🌍 The #RingOfFire experiences most of #Earth's volcanic #eruptions and #earthquakes.

    The activity is driven by #tectonic plates shifting and colliding over billions of years. Marie Tharp's #ocean floor mapping eventually provided the proof that confirmed continental drift.

    👉 Learn more: seethis.tv/post/tectonic-plate

    #20thcentury #cartography #geography #geology #geophysics #gravity #history #lava #maps #marianatrench #mountains #naturalhistory #pacific #pangea #rocks #science #underwater #volcanology #womeninstem #tksst #video

  44. 💁🏻‍♀️ ICYMI: 🌋🌍 The #RingOfFire experiences most of #Earth's volcanic #eruptions and #earthquakes.

    The activity is driven by #tectonic plates shifting and colliding over billions of years. Marie Tharp's #ocean floor mapping eventually provided the proof that confirmed continental drift.

    👉 Learn more: seethis.tv/post/tectonic-plate

    #20thcentury #cartography #geography #geology #geophysics #gravity #history #lava #maps #marianatrench #mountains #naturalhistory #pacific #pangea #rocks #science #underwater #volcanology #womeninstem #tksst #video