Images

A scientist from the Florence Bascom Geoscience Center performs field work in support of Task 2 of the Quaternary Geologic Mapping of the Glaciated Regions Project.

Photograph of a boulder (glacial drop stone) in Massachusetts taken during field work for Task 1.                                                                   

Figure adapted from Soller and Reheis (2004) showing the extent of the glaciated regions in the continental United States; blue star indicates the location of active (ongoing) USGS Quaternary geologic mapping at US Army Base Fort Drum, New York.

USGS scientists Brandon Graham, Grant Colip, and Shannon Mahan collect sediment samples at US Army Base Fort Drum, New York.

USGS scientist Shannon Mahan records notes at a field sampling site.                                                                                  

USGS Pathways intern Allison Kusick labels rotosonic sediment cores collected from a glacial lake in Jefferson County, Wisconsin.

Will Odom is a Research Geologist at the Florence Bascom Geoscience Center. Hiswork uses cosmogenic nuclide geochronology and AI-based mapping techniques to address geologic, tectonic, and geomorphologic questions.

An outcrop of greenschist-facies metamorphosed siltstone from the Roanoke Rapids terrane in southeastern Virginia.

This is a map showing the various different rock bodies of the Piedmont geologic province spanning Virginia, North and South Carolina, and Georgia.

Large pavement outcrop of granite in the Piedmont National Wildlife Refuge, Georgia.  These rocks may hold valuable mineral commodities, but such pavements also host unique and rare plant ecosystems.  Our work in Georgia provides critical geologic information for natural resource management. 

Mineralized silicified cataclasite (fault rock) from the Roanoke Rapids terrane in southeastern Virginia. This rock contains abundant pyrite, as well as traces of gold, silver, and telluride minerals. 

A paleoliquefaction sand dike in riverbank sediment along the Nottoway River in southeastern Virginia (the dike is the light-colored vertical feature between the shovel and the end of the sample tube). Such sand dikes may be the result of strong earthquakes.  We collected sediment in the tube for optically stimulated luminescence dating (conducted by the U

Photo of the Laser Diffraction Lab at the Florence Bascom Geoscience Center                                        

Logo for Paleoclimate Research: Integrating Systems and Models (PRISM5) project at Florence Bascom Geoscience Center

Project co-lead Harry Dowsett by Miocene sediments at Stratford Hall, VA in support of the Florence Bascom Geoscience Center

Project co-lead Marci Robinson by Pliocene sediments near Rushmere, VA in support of the Florence Bascom Geoscience Center

Scallop shells from the Miocene and Pliocene were as big as dinner plates         

A sediment core being measured and described at the drill site                   

Beckman Coulter LS 13 320 XR laser diffraction analyzer equipment housed in the Laser Diffraction Lab.

A photo of the Leica Z16 APO petrographic microscope equipment housed in the Laser Diffraction Lab

A photo of the Bruker S1 Titan portable X-ray fluorescence (XRF) instrumentation housed in the Laser Diffraction Lab.