Study confirms fossil footprints at White Sands National Park date to the Last Glacial Maximum
Geosciences and Environmental Change Science Center
Geosciences and Environmental Change Science Center (GECSC) researchers conduct multi-purpose geologic mapping and topical scientific studies to address issues concerning geologic, climatic, ecosystem, and land surface changes; human interactions with the environment; and physical, chemical, and biological characterization of the Earth's surface and upper crust.
News
Friday's Findings - April 26, 2024
Friday's Findings - April 26, 2024
Media Alert: USGS field crews to study avalanche prone regions using airborne techniques near Durango
Media Alert: USGS field crews to study avalanche prone regions using airborne techniques near Durango
In monarch butterfly decline mystery, scientists rule out habitat loss in migration zone
In monarch butterfly decline mystery, scientists rule out habitat loss in migration zone
Publications
Leveraging natural capital accounting to support businesses with nature-related risk assessments and disclosures
Nature loss threatens businesses, the global economy and financial stability. Understanding and addressing these risks for business will require credible measurement approaches and data. This paper explores how natural capital accounting (NCA) can support business data and information needs related to nature, including disclosures aligned with the Taskforce on Nature-related Financial Disclosures
Late Triassic paleogeography of southern Laurentia and its fringing arcs: Insights from detrital zircon U-Pb geochronology and Hf isotope geochemistry, Auld Lang Syne basin (Nevada, USA)
Fluvial strata of the Upper Triassic Chinle Formation and Dockum Group, exposed across the Western Interior of North America, have long been interpreted to record a transcontinental river system that connected the ancestral Ouachita orogen of Texas and Oklahoma, USA, to the Auld Lang Syne basin of northwestern Nevada, USA, its inferred marine terminus. Fluvial strata are well-characterized by exis
Recent advances in characterizing the crustal stress field and future applications of stress data: Perspectives from North America
The stress field controls patterns of crustal deformation, including which faults are likeliest to cause earthquakes or transmit fluids. Since the 1950s, maps of maximum horizontal stress (SHmax) orientations have advanced dramatically, and the style of faulting (relative principal stress magnitudes) has recently been mapped in some regions as well. This perspectives paper summarizes developments