Detection of source horizontal boundaries is a common feature in the interpretation of
magnetic and gravity data. A wide range of derivative-and phase-based methods are …

Determining lateral boundaries of the potential field source is a common feature in
interpreting magnetic and gravity data. There are many different phase based filters to …

Horizontal boundary identification of causative sources is an essential tool in potential field
data interpretation due to the feasibility of automatically retrieving the boundary information …

Abstract Topographic highs (“bumps”) across glaciated landscapes have the potential to
temporarily slow ice sheet flow or, conversely, accelerate ice flow through subglacial strain …

The seismic potential of crustal faults within the forearc of the northern Cascadia subduction
zone in British Columbia has remained elusive, despite the recognition of recent seismic …

Documenting spatial and temporal patterns of past landsliding is a challenging step in
quantifying the effect of landslides on landscape evolution. While landslide inventories can …

Several aspects of the earthquake characterization were changed for the Pacific Northwest
portion of the 2014 update of the national seismic hazard maps, reflecting recent scientific …

Subduction forearcs are subject to seismic hazard from upper plate faults that are often
invisible to instrumental monitoring networks. Identifying active faults in forearcs therefore …

High‐resolution aeromagnetic surveys of the Cascade Range and Yakima fold and thrust
belt (YFTB), Washington, provide insights on tectonic connections between forearc and back …

The fault‐related Yakima folds deform Miocene basalts and younger deposits of the
Columbia Plateau in central Washington State. Geodesy implies~ 2 mm/yr of NNE directed …