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Sand : its origin, transportation,abrasion and accumulation / Ph. H. Kuenen

By: Material type: TextTextLanguage: English Series: The Geological Society of South Africa; Annexure to Volume LXIIPublication details: Johannesburg : The Geological Society of South Africa, 1959Description: 33 pages : plates; 24 cmSubject(s): DDC classification:
  • REP 553.622 KUE
Summary: A small amount of sand is formed directly from magma by explosive activity of volcanoes. Calcerous particles of sand size are produced by organisms, especially yests of Foraminifera and Ostracod shells, or detritus from echinoderms, molluscs, brachipods, corals and such like
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Alex. L. du Toit Memorial Lectures, No. 6 Bibliography

A small amount of sand is formed directly from magma by explosive activity of volcanoes. Calcerous particles of sand size are produced by organisms, especially yests of Foraminifera and Ostracod shells, or detritus from echinoderms, molluscs, brachipods, corals and such like

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