Magnetic Fly Ash as a Chronological Marker in Post-Settlement Alluvial and Lacustrine Sediment: Examples from North Carolina and Illinois

Fly ash consists of mainly silt-size spherules that form during high-temperature coal combustion, such as in steam locomotives and coal-burning power plants. In the eastern USA, fly ash was distributed across the landscape atmospherically beginning in the late 19th century, peaking in the mid-20th c...

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Bibliographic Details
Main Authors: David A. Grimley, Ashley S. Lynn, Colby W. Brown, Neal E. Blair
Format: Article
Language:English
Published: MDPI AG 2021-04-01
Series:Minerals
Subjects:
Online Access:https://www.mdpi.com/2075-163X/11/5/476