My research interests are broadly focused around stratigraphic and tectonic characterization of sedimentary basins. I am interested in the evolution of sedimentary systems in the context of intrinsically-related regional tectonics in addition to grain-scale processes inferred from deposits.
My current research is focused on dispersal of sediment along the southern Cascadia margin, striving to understand the relationships between submarine mass failure events and sediment supply/source when tectonic or climatic changes impart imbalance on the stability of continental shelves. This work combines modern sediment cores, sediment provenance data, geochronology, and geophysical/remote sensing data to study regional tectonism, basin evolution, and stratigraphy, facilitating a better understanding of geohazards along the Cascadia margin.
Expertise
Sedimentology/stratigraphy, detrital geochronology, seafloor processes, tectonics
Professional Experience
2019–present: USGS Mendenhall Research Fellow, U.S. Geological Survey, Santa Cruz, CA
2017–2019: Postdoctoral Researcher, Stanford University/Monterey Bay Aquarium Research Institute (MBARI)
2014: Geoscience Intern, Chevron, Houston, Texas
2012: Geoscience Intern, ConocoPhillips, Houston, Texas
Education and Certifications
2017: Ph.D. – Geological & Environmental Sciences, Stanford University
2011: B.S. & B.A. – Geoscience & French, University of Utah
Science and Products
Science Seminar Series
Science Seminar Series Archives
U.S. West Coast and Alaska Marine Geohazards
Donated ROV vibracore and sampling data collected during Monterey Bay Aquarium Research Institute cruises in 2019 offshore of south-central California
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
Science Seminar Series
Welcome to the Pacific Coastal Marine Science Center (PCMSC) Seminar Series! Our seminars are on the first and third Tuesday of every month, usually from 10:00 – 11:00 am Pacific Time (1:00 - 2:00 pm Eastern) via Microsoft Teams. Please check each seminar announcement closely, as times may change. In addition, we also co-host a special “Coastal Change Hazards” seminar on the second Tuesday every...Science Seminar Series Archives
A list of past science seminars hosted by the Pacific Coastal and Marine Science Center, Santa Cruz, CaliforniaU.S. West Coast and Alaska Marine Geohazards
Marine geohazards are sudden and extreme events beneath the ocean that threaten coastal populations. Such underwater hazards include earthquakes, volcanic eruptions, landslides, and tsunamis. - Data
Donated ROV vibracore and sampling data collected during Monterey Bay Aquarium Research Institute cruises in 2019 offshore of south-central California
This dataset includes photographs of vibracores that were collected by the Monterey Bay Aquarium Research Institute (MBARI) in February 2019 and November 2019 aboard the R/V Western Flyer using the remotely operated vehicle (ROV) Doc Ricketts. The collection of these cores was funded entirely by MBARI, and the cores have been donated to the U.S. Geological Survey (USGS). The cores were collected i - Multimedia
- Publications
Sediment gravity flow frequency offshore central California diminished significantly following the Last Glacial Maximum
A high-resolution multibeam survey from a portion of the San Simeon Channel (offshore Morro Bay, California) captured a zone of recurring troughs and ridges adjacent to prominent submarine meander bends. Through an integrated study using surveying data, sediment core analysis, radiocarbon dating, and stable isotope measurements, we hypothesize that turbidity current event frequency was higher duriDetrital zircon provenance of the Cretaceous-Neogene East Coast Basin reveals changing tectonic conditions and drainage reorganization along the Pacific margin of Zealandia
The Upper Cretaceous–Pliocene strata of New Zealand record ~100 m.y. of Zealandia’s evolution, including development of the Hikurangi convergent margin and Alpine transform plate boundary. A comprehensive, new detrital zircon U-Pb data set (8315 analyses from 61 samples) was generated along a ~700 km transect of the East Coast Basin of New Zealand. Age distributions were analyzed and interpreted iLinking 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
- News