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  2. Lava dome - Wikipedia

    en.wikipedia.org/wiki/Lava_dome

    The former implies the enlargement of a lava dome due to the influx of magma into the dome interior, and the latter refers to discrete lobes of lava emplaced upon the surface of the dome. [2] It is the high viscosity of the lava that prevents it from flowing far from the vent from which it extrudes, creating a dome-like shape of sticky lava ...

  3. Laccolith - Wikipedia

    en.wikipedia.org/wiki/Laccolith

    A laccolith is a body of intrusive rock with a dome-shaped upper surface and a level base, fed by a conduit from below. A laccolith forms when magma (molten rock) rising through the Earth's crust begins to spread out horizontally, prying apart the host rock strata. The pressure of the magma is high enough that the overlying strata are forced ...

  4. Endogeny (biology) - Wikipedia

    en.wikipedia.org/wiki/Endogeny_(biology)

    For example, endogenous substances, and endogenous processes are those that originate within a living system (e.g. an organism or a cell). For instance, estradiol is an endogenous estrogen hormone produced within the body, whereas ethinylestradiol is an exogenous synthetic estrogen, commonly used in birth control pills .

  5. List of lava domes - Wikipedia

    en.wikipedia.org/wiki/List_of_lava_domes

    Lava domes are common features on volcanoes around the world. Lava domes are known to exist on plate margins as well as in intra-arc hotspots, and on heights above 6000 m and in the sea floor. [1] Individual lava domes and volcanoes featuring lava domes are listed below.

  6. Mono–Inyo Craters - Wikipedia

    en.wikipedia.org/wiki/Mono–Inyo_Craters

    [48]: 5 Mound-shaped features called lava domes are often created from these flows. Rock fragments thrown from a growing lava dome may reach 3.1 to 6.2 miles (5 to 10 km) from the dome. [ 47 ] A partial collapse of the steep-sided growing dome can send pyroclastic flows outward at least 3.1 miles (5 km). [ 47 ]

  7. Kīpuka - Wikipedia

    en.wikipedia.org/wiki/Kīpuka

    A kīpuka surrounded by lava flows at Kīlauea volcano, Hawai`i Green kīpukas surrounded by brown lava flows erupted from Iwate volcano, Japan. A kīpuka is an area of land surrounded by one or more younger lava flows. A kīpuka forms when lava flows on either side of a hill, ridge, or older lava dome as it moves downslope or spreads from its ...

  8. Heat wave or heat dome? Yes, there's a difference - AOL

    www.aol.com/news/heat-wave-heat-dome-yes...

    The term 'heat dome' has gained prominence recently as climate change, El Niño and other variables have warmed global temperatures and shifted weather patterns. Heat wave or heat dome? Yes, there ...

  9. Lava spine - Wikipedia

    en.wikipedia.org/wiki/Lava_spine

    A lava spine (or lava spire) is a vertical growth of solid lava that is forced from a volcanic vent. A lava spine can either be formed by viscous lava slowly being pushed out of the vent, or by magma that has solidified within the vent before being pushed out.

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