Publications
USGS research activities relevant to Alaska have yielded more than 9400 historical publications. This page features some of the most recent newsworthy research findings.
U.S. Geological Survey Benchmark Glacier Project
The U.S. Geological Survey Benchmark Glacier Project combines decades of direct glaciological data with remote sensing data to advance the quantitative understanding of glacier-climate interactions. The global loss of glaciers, and consequent implications for water resources, sea level rise, and ecosystem function underscores the importance of U.S. Geological Survey glaciology research to facilit
Divergent gene expression profiles in Alaskan sea otters: An indicator of chronic domoic acid exposure?
Temperature variations in the northern Gulf of Alaska across synoptic to century-long time scales
Evaluating hydrologic region assignment techniques for ungaged basins in Alaska, USA
Reproducibility and variability of earthquake subsidence estimates from saltmarshes of a Cascadia estuary
Sclerochronological records of environmental variability and bivalve growth in the Pacific Arctic
Proceedings of the Highly Pathogenic Avian Influenza and Wild Birds Webinar Series, August 2–5, 2021
Detrital zircon ages from upper Paleozoic–Triassic clastic strata on St. Lawrence Island, Alaska: An enigmatic component of the Arctic Alaska–Chukotka microplate
Modeled interactions of mountain pine beetle and wildland fire under future climate and management scenarios for three western US landscapes
Gull plumages are, and are not, what they appear to human vision
Evidence of increased mussel abundance related to the Pacific marine heatwave and sea star wasting
Marine minerals in Alaska — A review of coastal and deep-ocean regions
Minerals occurring in marine environments span the globe and encompass a broad range of mineral categories, forming within varied geologic and oceanographic settings. They occur in coastal regions, either from the continuation or mechanical reworking of terrestrial mineralization, as well as in the deep ocean, from diagenetic, hydrogenetic, and hydrothermal processes. The oceans cover most of the