Drainage networks that have formed by ground-water sapping are develop
ed in the highly permeable sands of the Citronelle Formation in the Fl
orida Panhandle. The valleys resemble those formed on Hawaii, the Colo
rado Plateau and on Mars, but they have developed without significant
lithologic controls. Drainage patterns range from trellis to dendritic
depending on the effect of beach ridges and relative relief. Many of
the drainage networks are not fully developed, and the adjacent upland
s have been modified by marine, aeolian, and to a limited extent fluvi
al processes. Extension of the networks appears to be episodic, as a r
esult of fires, hurricanes, and human activities, which damage or dest
roy vegetation.