Abstract The Mississippi River fluvial–marine sediment-dispersal system (MRS) has become
the focus of renewed research during the past decade, driven by the recognition that the …

Abstract Large earthquakes in North China, Australia, Northwestern Europe, Central and
Eastern United States, and other mid-continents show complex spatiotemporal patterns that …

Large earthquakes within stable continental regions (SCR) show that significant amounts of
elastic strain can be released on geological structures far from plate boundary faults, where …

Fluvial deposits and landforms are important archives of river response to climate, tectonics
and base level change and are commonly associated with archaeological sites. Unlike …

One of the most powerful features of plate tectonics is that the known plate motions give
insight into both the locations and average recurrence interval of future large earthquakes …

Surface-rupturing earthquakes can produce fault displacements that abruptly alter the
established course of rivers. Several notable examples of fault rupture–induced river …

The three-dimensional reconstruction of meander-belt deposits from ancient strata provides
insight into the formative processes of meander-bend evolution and paleogeographic …

The lower Mississippi valley contains multiple large braid belts for which age control has
been limited. Application of the optically stimulated luminescence technique has produced a …

Long records often show large earthquakes occurring in supercycles, sequences of
temporal clusters of seismicity, cumulative displacement, and cumulative strain release …

We recover the Holocene earthquake history of seven seismogenic normal faults in the
Fucino system, central Italy. We collected 800 samples from the wellpreserved limestone …