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  2. Pseudomorph - Wikipedia

    en.wikipedia.org/wiki/Pseudomorph

    Silica pseudomorph after gypsum crystals and silicified serpulid polychaete tubes Pseudomorph of goethite after pyrite. In mineralogy, a pseudomorph is a mineral or mineral compound that appears in an atypical form (crystal system), resulting from a substitution process in which the appearance and dimensions remain constant, but the original mineral is replaced by another due to alteration, or ...

  3. Permineralization - Wikipedia

    en.wikipedia.org/wiki/Permineralization

    Permineralization, a type of fossilization, involves deposits of minerals within the cells of organisms. Water from the ground, lakes, or oceans seeps into the pores of organic tissue and forms a crystal cast with deposited minerals. Crystals begin to form in the porous cell walls.

  4. Fossil - Wikipedia

    en.wikipedia.org/wiki/Fossil

    A derived, reworked or remanié fossil is a fossil found in rock that accumulated significantly later than when the fossilized animal or plant died. [100] Reworked fossils are created by erosion exhuming (freeing) fossils from the rock formation in which they were originally deposited and their redeposition in a younger sedimentary deposit.

  5. Water Resistant mark - Wikipedia

    en.wikipedia.org/wiki/Water_Resistant_mark

    The watch shall be placed on a heated plate at a temperature between 40 °C and 45 °C until the watch has reached the temperature of the heated plate (in practice, a heating time of 10 minutes to 20 minutes, depending on the type of watch, will be sufficient). A drop of water, at a temperature between 18 °C and 25 °C shall be placed on the ...

  6. Understanding the Sixth Sense of the Platypus - AOL

    www.aol.com/lifestyle/understanding-sixth-sense...

    While most modern mammals begin showing up in fossil records dating back 60 million years, monotremes are thought to have evolved around 130 million years ago. How the Platypus Uses Its Sixth ...

  7. Fractional crystallization (geology) - Wikipedia

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

    Fractional crystallization, or crystal fractionation, is one of the most important geochemical and physical processes operating within crust and mantle of a rocky planetary body, such as the Earth. It is important in the formation of igneous rocks because it is one of the main processes of magmatic differentiation . [ 1 ]