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  2. Eusideroxylon - Wikipedia

    en.wikipedia.org/wiki/Eusideroxylon

    Eusideroxylon are canopy tree species with erect or spreading branches and extremely durable and decay-resistant wood.. Eusideroxylon zwageri is a slow growing (0.5 metres per year) [4] [5] tall evergreen tree with a straight bole (usually host to Cassytha, a parasitic vine with leaves reduced to scales, up to half of the tree's height).

  3. Charcoal iron - Wikipedia

    en.wikipedia.org/wiki/Charcoal_iron

    Charcoal iron is the substance created by the smelting of iron ore with charcoal. All ironmaking blast furnaces were fueled by charcoal until Abraham Darby introduced coke as a fuel in 1709. The more economical coke soon replaced charcoal in British furnaces, but in the United States , where timber for charcoal was abundant, charcoal furnaces ...

  4. British timber trade - Wikipedia

    en.wikipedia.org/wiki/British_timber_trade

    It would be many decades, however, before iron could be used to replace timber in shipbuilding. By the eighteenth-century England had not exhausted its supply of suitable domestic hardwood timber but – like the Netherlands – it imported softwood supplies. While every nation has trees and wood, ship timber is a far more limited product.

  5. Petrifaction - Wikipedia

    en.wikipedia.org/wiki/Petrifaction

    Tree remains that have undergone petrifaction, as seen in Petrified Forest National Park. In geology, petrifaction or petrification (from Ancient Greek πέτρα (pétra) 'rock, stone') is the process by which organic material becomes a fossil through the replacement of the original material and the filling of the original pore spaces with minerals.

  6. 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 ...

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