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  2. Thrihnukagigur - Wikipedia

    en.wikipedia.org/wiki/Thrihnukagigur

    Covering a 3,270 square metres (35,200 sq ft) area and a depth of 213 meters (699 ft), [2] it has not erupted in the past 4000 years. [3] It was discovered in 1974 by cave explorer Árni B. Stefánsson, and opened for tourism in 2012. It is the only volcano in the world where visitors can take an elevator and safely descend into the magma chamber.

  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. Stoping (geology) - Wikipedia

    en.wikipedia.org/wiki/Stoping_(geology)

    Once suspended in the melt, stoped blocks may either sink or float depending upon the density of the block relative to that of the melt. Additionally, blocks submerged within melt are subject to further thermally-induced fracturing which may account for the often observed "lack of evidence" for the process of stoping.

  5. Iceland volcano – live: Experts reveal exact location for ...

    www.aol.com/news/iceland-volcano-live-experts...

    Iceland’s new #1 selfie spot may have emerged out of ground despite volcano threat. Blue Lagoon: ‘It is still impossible to determine if, when, or where an eruption might occur'

  6. 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

  7. Intrusive rock - Wikipedia

    en.wikipedia.org/wiki/Intrusive_rock

    Intrusive rock is formed when magma penetrates existing rock, crystallizes, and solidifies underground to form intrusions, such as batholiths, dikes, sills, laccoliths, and volcanic necks. [1] [2] [3] Intrusion is one of the two ways igneous rock can form. The other is extrusion, such as a volcanic eruption or similar event.

  8. Harmonic tremor - Wikipedia

    en.wikipedia.org/wiki/Harmonic_tremor

    Seismograph recording of harmonic tremor Four major types of seismograms, or seismic signatures. A harmonic tremor is a sustained release of seismic and infrasonic energy typically associated with the underground movement of magma, the venting of volcanic gases from magma, or both in volcanoes, and with repetitive stick-slip or other impulsive activity in non-volcanic systems.

  9. Resolution Copper - Wikipedia

    en.wikipedia.org/wiki/Resolution_copper

    By early 2023, more than $2 billion had been spent on exploratory work and preparation for the project. [6] Resolution Copper also owns the mineral rights acquired from ASARCO to the Superior East deposit which is another deep-seated Porphyry copper deposit within a mile to the east. [7] [8]