Abstract
Due to long-lasting tradition of coal mining and industrial history on the territory of Czech Republic, significant amount of waste piles of various ages and scales occur. Many of them, along with scarce occurrences of naturally burned coal measures, spontaneously ignited and subsequently, served as a source of diverse assemblage of newly formed minerals – products of pyrometamorphism, alteration, and sublimation. Several new minerals associated with combustion metamorphism were first described from the Czech Republic: tschermigite (1853), rosickýite (1931), letovicite (1932), kratochvílite (1937), kladnoite (1942), koktaite (1948), and rostite (1979). This chapter mainly focuses on two most famous localities, both situated to the Carboniferous sedimentary basins: Kladno Coal District in Central Bohemia near the capital Prague and Radvanice at Trutnov in Eastern Bohemia, close to border with Poland. These two localities, which were studied in detail, provided nearly 100 recently formed minerals and unnamed compounds.
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