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  2. Effusive eruption - Wikipedia

    en.wikipedia.org/wiki/Effusive_eruption

    For an effusive eruption to occur, magma must be permeable enough to allow the expulsion of gas bubbles contained within it. If the magma is not above a certain permeability threshold, it cannot degas and will erupt explosively. Additionally, at a certain threshold, fragmentation within the magma can cause an explosive eruption.

  3. Volcanic and igneous plumbing systems - Wikipedia

    en.wikipedia.org/wiki/Volcanic_and_igneous...

    Magma emplacement can take place at any depth above the source rock. [4] Magma emplacement is primarily controlled by the internal forces of magma including buoyancy and magma pressure. [2] Magma pressure changes with depth as vertical stress is a function of the depth. [20] Another parameter of magma emplacement is the rate of magma supply. [2]

  4. Magma chamber - Wikipedia

    en.wikipedia.org/wiki/Magma_chamber

    Magma chambers above a subducting plate. Magma rises through cracks from beneath and across the crust because it is less dense than the surrounding rock. When the magma cannot find a path upwards it pools into a magma chamber. These chambers are commonly built up over time, [4] [5] by successive horizontal [6] or vertical [7] magma injections

  5. Deep Core (film) - Wikipedia

    en.wikipedia.org/wiki/Deep_Core_(film)

    They eject the bomb pod from the main mining vehicle, but Alan stays in the pod and delays the self-destruct by tying up the computer with a diagnostics program. Brian and his team find a magma flow, to get them to the surface away from the nuclear bombs before they detonate. The nuclear bombs all explode successfully.

  6. Phreatomagmatic eruption - Wikipedia

    en.wikipedia.org/wiki/Phreatomagmatic_eruption

    The Minoan eruption had four phases. Phase 1 was a white to pink pumice fallout with dispersal axis trending ESE. The deposit has a maximum thickness of 6 m and ash flow layers are interbedded at the top. Phase 2 has ash and lapilli beds that are cross stratified with mega-ripples and dune-like structures. The deposit thicknesses vary from 10 ...

  7. Strombolian eruption - Wikipedia

    en.wikipedia.org/wiki/Strombolian_eruption

    The most energetic Strombolian eruptions are sometimes termed "Violent Strombolian" by volcanologists. [2] Such eruptions are associated with higher magma gas content, leading to a turbulent churn flow regime in the conduit, producing stronger and much more frequent explosions.

  8. Book Review: 'The Spice Must Flow' chronicles the legacy of ...

    www.aol.com/entertainment/book-review-spice-must...

    The saga of how cult sci-fi novel “Dune” slowly permeated the mainstream over decades is a tale with almost as many twists and turns as “Dune” itself, and author Ryan Britt recounts it in ...

  9. Fractional crystallization (geology) - Wikipedia

    en.wikipedia.org/wiki/Fractional_crystallization...

    Cumulate rock – Igneous rocks formed by the accumulation of crystals from a magma either by settling or floating. Flow banding – Bands or layers that can sometimes be seen in rock that formed from magma; Fractional crystallization (chemistry) – Method for refining substances based on differences in their solubility