Anthracite iron century. Research into the smelting of iron using anthracite coal (without coking it first) began in the 1820s in Wales by Thomas, experiments in France, most notably by Gueymard and Robin at Vizille in 1827, and in the 1830s in Pottsville & Mauch Chunk, Pennsylvania. Early attempts tried to gradually substitute anthracite for other fuels, such as coke or charcoal, but all failed due to the use of cold blast techniques, which generated insufficient heat to keep the anthracite in regenerative combustion. In the same time-frame, Thomas had also continued experimenting with mixes of Anthracite and other fuels, before he
Anthracite budgerigar mutation the Anthracite locus. This darkens the body colour to a shade somewhat deeper than a Dark Green. The DF Anthracite Light Green, with two Anthracite alleles, is a deep olive colour. In the blue series varieties the SF Anthracite Skyblue has one Anthracite allele and one wild-type allele, with a body colour rather like a deep Cobalt. The DF Anthracite Skyblue with two Anthracite alleles, the true Anthracite variety, has a dark grey, almost black, body colour with mauve overtones. Because the Anthracite factor is always visibly expressed no budgerigar can be split for Anthracite. The heterozygotes of Anthracite with