I have a spectacular up to 2m-scale colonnade structure by clay deposits of an ancient deltaic sedimentary environments. It is similar to the cooling columnar joints of volcanics and volcaniclastics or sandstone in thermal contact. l described this occurrence as the first record within the clay. I would like to be sure of that ?

it is not surficial or sub-aerial like desiccation mud crack features.

More Mohamed Saleh Hassan Hammed's questions See All
Similar questions and discussions