An angular unconformity therefore exists along the anticline's crest.
The major axis is determined by an anticline.
Another anticline has been mapped to the north of this ring syncline, which is also concentric with it.
The fontanili line is the outcrop, or intersection, of the anticline's water table with the surface at the edge of the "bassa".
The valley is a collapsed anticline, a type of geological fold.
The orebodies are on one limb of a plunging anticline and are extensively faulted.
In a symmetrical anticline, a surface trace of the axial plane coincides with the crest.
There are three mineral beds which are between 2.5 and 8 m thick which are folded in an anticline that plunges to the south-west.
