Morphometric analysis of a reactivated Variscan fault in the southern Bohemian Massif (Budějovice basin, Czech Republic)

The analysed part of the margin of the Budějovice basin that is not fault controlled revealed geomorphic parameters that are not indicative for differential vertical displacements (Smf 1.30 to 4,16, SL up to 57, Vf 2.10 to 4.80). Concave-up stream profiles of creeks draining into the basin are characteristic for equilibrated streams.