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Most of Slovenia's intricate fluvial network is directed toward the Danube River.
Rivers are known to respond to changes in the rate of rock uplift by propagating knickpoints through the fluvial network.
During the Etruscan and Roman periods, Pisa saw a fast urban expansion in a dense and unstable fluvial network.
A recent regional uplift controlled the organization of the present fluvial network and dissection of the landscape.
The crater is a drainage basin for a ~90 km-long fluvial network where the channel system debouches into the crater.
On the other hand, the entire fluvial network should be modified by the sea level changes of the Black Sea, particularly in the late Quaternary.
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Rejuvenation of fluvial networks by channel incision often leads to further network development and an increase in drainage density as gullies migrate into previously non-incised surfaces.
Rejuvenation of fluvial networks by channel incision generally leads to further network development and an increase in drainage density as gullies migrate into previously nonincised surfaces.
Currently, there is a need for more highly resolved studies at stream and river scales that enable estimates of terrestrial carbon turnover within fluvial networks.
On Earth, fluvial networks with strongly preferred orientations are often associated with structural features, such as faults or joints, that influence flow or erodibility.
We validated our modified algorithm by applying it to synthetic fluvial networks produced by a landscape evolution model with no structural control of drainage orientations, and confirmed that only a small fraction of the networks are falsely identified as structurally controlled.
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