In NW Europe, chalk areas are generally covered with clay-with-flints (CWF)
. These formations are made of flints with a clayey or silty-clayey matrix.
In the literature devoted to CWF, the flint dissolution during the weather
ing of chalk was poorly studied. In this study, we provide an estimation of
this phenomenon in the western Paris Basin, by comparisons between the fli
nts of CWF and those of chalks based on mineralogy, size, cortex and surfac
e cavities of flints.
Our results show that the mineralogy and thickness of flints have not been
affected by the weathering. Only the volumes of cortex and surface cavities
have increased. These two parametres allow us to quantify the flint dissol
ution. Flint dissolution is low : the amount of dissolved silica in flints
varies between 0.9 and 7.3 %. These low values show that weathering of chal
k who has led to the creation of CWF has not reached the intensity of a lat
eritic type weathering, as is the case in the ferralitic soil.