The New Jersey Sea Level Transect was designed to evaluate the relationships among
global sea level (eustatic) change, unconformity‐bounded sequences, and variations in …

The persistence of topography within ancient orogens remains one of the outstanding
questions in landscape evolution. In the eastern North American Appalachians, this question …

Bedrock fluvial incision and longitudinal profile development over geologic time scales
determined by fluvial terraces Page 215 Bedrock Fluvial Incision and Longitudinal Profile …

For nearly a century, the Atlantic Coastal Plain (ACP) of the United States has been the
focus of studies investigating Pliocene and Pleistocene shorelines, however, the mapping of …

We integrate existing and new geologic data [REtreating TRench, Extension, and Accretion
Tectonics (RETREAT project)], particularly on the origin, growth, and activity of the mountain …

We have reconstructed the Oligocene to Middle Miocene paleobathymetry and stratigraphy
of the New Jersey margin using a modified backstripping technique. By analyzing the …

The Pliocene epoch represents an important transition from a climate regime with high-
frequency, low-amplitude oscillations when the Northern Hemisphere lacked substantial ice …

A perplexing macrogeomorphic problem is the persistence of topography in mountain
ranges that were initially formed by orogenic events hundreds of millions of years old. In this …

Despite the century‐long recognition of regional epeirogeny along the middle Atlantic
passive margin, relatively few studies have focused on understanding postrift uplift …

High-frequency Quaternary glacioeustasy resulted in the incision of six moderate-to high-
relief fluvial erosion surfaces beneath the Virginia inner shelf and coastal zone along the …