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  2. Theraphosinae - Wikipedia

    en.wikipedia.org/wiki/Theraphosinae

    The Theraphosinae are a large subfamily of Mygalomorphae spiders in the family Theraphosidae found primarily in the Neotropical realm. Genera

  3. List of Theraphosidae species - Wikipedia

    en.wikipedia.org/wiki/List_of_Theraphosidae_species

    Main page; Contents; Current events; Random article; About Wikipedia; Contact us

  4. Phreatomagmatic eruption - Wikipedia

    en.wikipedia.org/wiki/Phreatomagmatic_eruption

    A further control on the morphology and characteristics of a deposit is the water to magma ratio. It is considered that the products of phreatomagmatic eruptions are fine grained and poorly sorted where the magma/water ratio is high, but when there is a lower magma/water ratio the deposits may be coarser and better sorted. [4]

  5. Magnacarina - Wikipedia

    en.wikipedia.org/wiki/Magnacarina

    This Theraphosidae -related article is a stub. You can help Wikipedia by expanding it.

  6. Tmesiphantes - Wikipedia

    en.wikipedia.org/wiki/Tmesiphantes

    Tmesiphantes is a genus of Brazilian tarantulas in the subfamily Theraphosinae that was first described by Eugène Louis Simon in 1892. [ 1 ] [ 2 ] The genera Magulla and Melloleitaoina were brought into synonymy in 2019.

  7. Magma - Wikipedia

    en.wikipedia.org/wiki/Magma

    Magma that cools slowly within a magma chamber usually ends up forming bodies of plutonic rocks such as gabbro, diorite and granite, depending upon the composition of the magma. Alternatively, if the magma is erupted it forms volcanic rocks such as basalt , andesite and rhyolite (the extrusive equivalents of gabbro, diorite and granite ...

  8. 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

  9. Ultrapotassic igneous rocks - Wikipedia

    en.wikipedia.org/wiki/Ultrapotassic_igneous_rocks

    carbon dioxide or water (each condition leading to a distinctive magma); reaction of melts with surrounding rock as they rise from their sources; Mantle sources of ultrapotassic magmas may contain subducted sediments, or the sources may have been enriched in potassium by melts or fluids partly derived from subducted sediments.