USGS scientists on the back deck of M/V Bold Horizon in San Francisco Bay: (back row, standing: left to right) Brandon Nasr, Danny Brothers, Travis Alonghi (USGS student contractor), Gerry Hatcher, Jenna Hill, Pete Dal Ferro, and Jenny McKee; (front row, kneeling: left to right) USGS scientists Janet Watt and Nora Nieminski.
Nora Nieminski (Former Employee)
Science and Products
Science Seminar Series Archives
Coastal and Marine Geohazards of the U.S. West Coast and Alaska
Sediment core data from offshore southern Cascadia during field activity 2019-643-FA
Compiled onshore and offshore paleoseismic data along the Cascadia Subduction zone
Radiocarbon age dating of biological material from cores collected off central California in 1999, 2006, and 2019
Multichannel minisparker seismic-reflection and chirp subbottom data collected offshore Northern California during USGS field activity 2019-643-FA
Donated ROV vibracore and sampling data collected during Monterey Bay Aquarium Research Institute cruises in 2019 offshore of south-central California
USGS scientists on the back deck of M/V Bold Horizon in San Francisco Bay: (back row, standing: left to right) Brandon Nasr, Danny Brothers, Travis Alonghi (USGS student contractor), Gerry Hatcher, Jenna Hill, Pete Dal Ferro, and Jenny McKee; (front row, kneeling: left to right) USGS scientists Janet Watt and Nora Nieminski.
Pockmarks offshore Big Sur, California provide evidence for recurrent, regional, and unconfined sediment gravity flows
Spatial distribution and variability of lobe facies in a large sand-rich submarine fan system: Neoproterozoic Zerrissene Group, Namibia
Time-lapse seafloor surveys reveal how turbidity currents and internal tides in Monterey Canyon interact with the seabed at centimeter-scale
Sediment gravity flow frequency offshore central California diminished significantly following the Last Glacial Maximum
Detrital zircon provenance of the Cretaceous-Neogene East Coast Basin reveals changing tectonic conditions and drainage reorganization along the Pacific margin of Zealandia
Linking direct measurements of turbidity currents to submarine canyon-floor deposits
Submarine canyons are conduits for episodic and powerful sediment density flows (commonly called turbidity currents) that move globally significant amounts of terrestrial sediment and organic carbon into the deep sea, forming some of the largest sedimentary deposits on Earth. The only record available for most turbidity currents is the deposit they leave behind. Therefore, to understand turbidity
Science and Products
Science Seminar Series Archives
Coastal and Marine Geohazards of the U.S. West Coast and Alaska
Sediment core data from offshore southern Cascadia during field activity 2019-643-FA
Compiled onshore and offshore paleoseismic data along the Cascadia Subduction zone
Radiocarbon age dating of biological material from cores collected off central California in 1999, 2006, and 2019
Multichannel minisparker seismic-reflection and chirp subbottom data collected offshore Northern California during USGS field activity 2019-643-FA
Donated ROV vibracore and sampling data collected during Monterey Bay Aquarium Research Institute cruises in 2019 offshore of south-central California
USGS scientists on the back deck of M/V Bold Horizon in San Francisco Bay: (back row, standing: left to right) Brandon Nasr, Danny Brothers, Travis Alonghi (USGS student contractor), Gerry Hatcher, Jenna Hill, Pete Dal Ferro, and Jenny McKee; (front row, kneeling: left to right) USGS scientists Janet Watt and Nora Nieminski.
USGS scientists on the back deck of M/V Bold Horizon in San Francisco Bay: (back row, standing: left to right) Brandon Nasr, Danny Brothers, Travis Alonghi (USGS student contractor), Gerry Hatcher, Jenna Hill, Pete Dal Ferro, and Jenny McKee; (front row, kneeling: left to right) USGS scientists Janet Watt and Nora Nieminski.
Pockmarks offshore Big Sur, California provide evidence for recurrent, regional, and unconfined sediment gravity flows
Spatial distribution and variability of lobe facies in a large sand-rich submarine fan system: Neoproterozoic Zerrissene Group, Namibia
Time-lapse seafloor surveys reveal how turbidity currents and internal tides in Monterey Canyon interact with the seabed at centimeter-scale
Sediment gravity flow frequency offshore central California diminished significantly following the Last Glacial Maximum
Detrital zircon provenance of the Cretaceous-Neogene East Coast Basin reveals changing tectonic conditions and drainage reorganization along the Pacific margin of Zealandia
Linking direct measurements of turbidity currents to submarine canyon-floor deposits
Submarine canyons are conduits for episodic and powerful sediment density flows (commonly called turbidity currents) that move globally significant amounts of terrestrial sediment and organic carbon into the deep sea, forming some of the largest sedimentary deposits on Earth. The only record available for most turbidity currents is the deposit they leave behind. Therefore, to understand turbidity