Deformation by Ice Push of Lithified Sediments in South-Central Iowa

Superficial structures attributed to deformation by ice push have developed in Pennsylvanian rocks exposed in Madison County, Iowa. Folds, faults, and joints are found in a lithified limestone and in underlying shale units, with deformation through flowage and fracture expressed in varying degrees i...

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Veröffentlicht in:The Journal of geology 1957-09, Vol.65 (5), p.546-550
Hauptverfasser: Lamerson, Paul R., Dellwig, Louis F.
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container_issue 5
container_start_page 546
container_title The Journal of geology
container_volume 65
creator Lamerson, Paul R.
Dellwig, Louis F.
description Superficial structures attributed to deformation by ice push have developed in Pennsylvanian rocks exposed in Madison County, Iowa. Folds, faults, and joints are found in a lithified limestone and in underlying shale units, with deformation through flowage and fracture expressed in varying degrees in the different lithologic units.
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source Jstor Complete Legacy
subjects Anticlines
Deformation
Geological Notes
Geology
Glacial till
Ice
Limestones
Quarries
Sediments
Shales
Stone
title Deformation by Ice Push of Lithified Sediments in South-Central Iowa
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