Research Article
Jun 1976
New York’s Glacial Lake Formation of Varved Silt and Clay
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VIEW THE REPLYPublication: Journal of the Geotechnical Engineering Division
Volume 102, Issue 6
Abstract
The principal and distinct subsoil of New York City is a varved glacial lake formation. While this formation has been considered, for many years, unsatisfactory for the support of heavy structures, laboratory testing of samples from the formation have demonstrated that it has been heavily preconsolidated. Settlement analyses have indicated that medium to high-rise structures accordingly may be supported above it with tolerable settlements. This paper presents the analyses and observations of settlement on a number of structures so supported and analyzes the conclusions derived from such observations regarding consolidation of the deposit and settlement of structures.
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Published In
Journal of the Geotechnical Engineering Division
Volume 102 • Issue 6 • June 1976
Pages: 605 - 638
Copyright
© 1976 American Society of Civil Engineers.
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Published in print: Jun 1976
Published online: Feb 11, 2021
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Authors
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James D. Parsons, F.ASCE
Consulting Engr., Asheville, N.C.; formerly, Assoc. Part. and Sr. Assoc., Mueser, Rutledge, Wentworth & Johnston, New York, N.Y.
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ASCE Library Cards let you download journal articles, proceedings papers, and available book chapters across the entire ASCE Library platform. ASCE Library Cards remain active for 24 months or until all downloads are used. Note: This content will be debited as one download at time of checkout.
Terms of Use: ASCE Library Cards are for individual, personal use only. Reselling, republishing, or forwarding the materials to libraries or reading rooms is prohibited.
Terms of Use: ASCE Library Cards are for individual, personal use only. Reselling, republishing, or forwarding the materials to libraries or reading rooms is prohibited.