Abstract
Gravels and other sedimentary materials on alternately flooded and dried high tidal flats show physical and chemical breakdown. Physical disintegration is by crystal wedging. Chemical weathering is promoted by high pH and Eh conditions with frequent leaching by tidal waters.
This content is PDF only. Please click on the PDF icon to access.
You do not have access to this content, please speak to your institutional administrator if you feel you should have access.