Collapsed and non‐collapsed ice‐marginal glaciodeltaic morphosequence structure mapped with ground penetrating radar in central Connecticut

ABSTRACT Glacial ice from the last major advance covered the state of Connecticut and reached its glacial maximum on Long Island ∼21,000 years ago. As glacial ice melted and retreated northward, meltwater streams deposited sediments, like gravel, sand, silt and clay, in low‐lying areas. Many perigla...

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Veröffentlicht in:	Near surface geophysics (Online) 2021-10, Vol.19 (5), p.583-602
Hauptverfasser:	Bouali, El Hachemi, Sweeney, Charles
Format:	Artikel
Sprache:	eng
Schlagworte:	Ground‐penetrating radar Near‐surface Shallow subsurface
Online-Zugang:	Volltext
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