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Understanding Chert in the Mid-Hudson Valley: A Note on a …

WebCherts occur in a variety of geological settings, for example: - Bedded cherts may form by compaction and recrystallization of silica-rich biogenic sediments made of opaline tests of single-cell organisms (diatoms, radiolaria) or remains of silicious sponges, both in marine and in lake environments. During diagenesis, the silica in the ... WebThere are, of course, other blue-gray cherts in the midwest and many of them can overlap Cobden-Dongola and Wyandotte cherts (see Tankersley 1984:254 for a list of eight such cherts). However, less confusion exists about these cherts, perhaps because they have been identified more recently in the context of modern chert source studies. closing remarks for career guidance program

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WebCherts occur in a variety of geological settings, for example: - Bedded cherts may form by compaction and recrystallization of silica-rich biogenic sediments made of opaline tests of single-cell organisms (diatoms, radiolaria) or remains of silicious sponges, both in marine and in lake environments. During diagenesis, the silica in the ... WebA new classification scheme for non-detrital siliceous rocks is proposed, facts and problems coneerning the origin of cherts are discussed, and a new genetic model is presented. The relationship between opal-and quartz-silica phases is discussed, and it is suggested that most of the quartz cherts originated from opaline precursors. The diagenetic opal/quartz … WebChert ( / ˈtʃɜːrt /) is a hard, fine-grained sedimentary rock composed of microcrystalline or cryptocrystalline quartz, [1] the mineral form of silicon dioxide (SiO 2 ). [2] Chert is characteristically of biological origin, but … closing remarks for church anniversary