Recent Surface Rupturing Earthquakes along the South Flank of the Greater Caucasus near Tbilisi, Georgia

Tectonostratigraphy and major structures of the Georgian Greater Caucasus: Implications for structural architecture, along-strike continuity, and orogen evolution

Late Holocene Slip Rate of the Mojave Section of the San Andreas Fault near Palmdale, California

Probabilistic Seismic Hazard Assessment Using Legacy Data in Georgia

Middle Miocene reorganization of the Altyn Tagh fault system, northern Tibetan Plateau

Magnetostratigraphy of the Ganyanchi (Salt Lake) Basin along the Haiyuan fault, northeastern Tibet

Drainage network reveals patterns and history of active deformation in the eastern Greater Caucasus

Point-based computing on scanned terrain with LidarViewer

Interactive terrain visualization enables virtual field work during rapid scientific response to the 2010 Haiti earthquake

Discovering marine terraces using airborne LiDAR along the Mendocino-Sonoma coast, northern California

A terrestrial lidar-based workflow for determining three–dimensional slip vectors and associated uncertainties

Faulted terrace risers place new constraints on the late Quaternary slip rate for the central Altyn Tagh fault, northwest Tibet

Cenozoic right-slip faulting along the eastern margin of the Pamir salient, northwestern China

Low Quaternary slip rate reconciles geodetic and geologic rates along the Altyn Tagh fault, northwestern Tibet

The Akato Tagh bend along the Altyn Tagh fault, northwest Tibet 1: Smoothing by vertical-axis rotation and the effect of topographic stresses on bend-flanking faults

The Akato Tagh bend along the Altyn Tagh fault, northwest Tibet 2: Active deformation and the importance of transpression and strain hardening within the Altyn Tagh system

Late Holocene earthquake history of the central Altyn Tagh fault, China

Is the North Altyn fault part of a strike-slip duplex along the Altyn Tagh fault system?

Range-front fault scarps of the Sierra El Mayor, Baja California: Formed above an active low-angle normal fault?