Jessica E. Pilarczyk

ORCID: 0000-0003-1127-1503
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About
Contact & Profiles
Research Areas
  • earthquake and tectonic studies
  • Geology and Paleoclimatology Research
  • Geological and Geophysical Studies
  • Methane Hydrates and Related Phenomena
  • Marine and environmental studies
  • Tropical and Extratropical Cyclones Research
  • Geological formations and processes
  • Coastal and Marine Dynamics
  • Pacific and Southeast Asian Studies
  • Seismology and Earthquake Studies
  • Coastal wetland ecosystem dynamics
  • Geological and Geochemical Analysis
  • Earthquake and Tsunami Effects
  • Landslides and related hazards
  • Earthquake and Disaster Impact Studies
  • Marine Biology and Ecology Research
  • Marine and fisheries research
  • Maritime and Coastal Archaeology
  • Flood Risk Assessment and Management
  • Island Studies and Pacific Affairs
  • Coastal and Marine Management
  • Isotope Analysis in Ecology
  • Environmental Engineering and Cultural Studies
  • Disaster Management and Resilience
  • 3D Modeling in Geospatial Applications

Simon Fraser University
2018-2023

University of Southern Mississippi
2016-2021

Stennis Space Center
2016-2021

Geological Survey of Japan
2019-2021

National Institute of Advanced Industrial Science and Technology
2019-2021

Institute of Marine and Coastal Research
2018

Rutgers, The State University of New Jersey
2014-2016

Earth Observatory of Singapore
2014-2016

Nanyang Technological University
2014-2016

UNSW Sydney
2012-2014

Abstract The devastating 2004 Indian Ocean tsunami caught millions of coastal residents and the scientific community off-guard. Subsequent research in basin has identified prehistoric tsunamis, but timing recurrence intervals such events are uncertain. Here we present an extraordinary 7,400 year stratigraphic sequence deposits from a cave Aceh, Indonesia. This record demonstrates that at least 11 tsunamis struck Aceh coast between 2,900 years ago. average time period is about 450 with...

10.1038/ncomms16019 article EN cc-by Nature Communications 2017-07-19

Abstract We present stratigraphic, archeological and historical evidence for two closely timed predecessors of the giant 2004 tsunami on northern coast Aceh, Sumatra. This is first direct that a played role in fifteenth century cultural hiatus along Sumatran portion maritime silk route. One seacliff exposure eastern side Lambaro headlands reveals beds tsunamigenic coral rubble within small alluvial fan. Radiocarbon Uranium‐Thorium disequilibrium dates indicate emplacement after 1344 ± 3 C.E....

10.1002/2014jb011538 article EN cc-by-nc-nd Journal of Geophysical Research Solid Earth 2014-12-13

Marine inundation associated with the 5 to 8 m storm surge of Typhoon Haiyan in 2013 left overwash sediments inland on coastal plains northwestern shores Leyte Gulf, Philippines. The deposit provides a modern sedimentary record deposition from Category landfalling typhoon. We studied at two locations that experienced similar conditions but represent contrasting sedimentological regimes, namely siliciclastic coast and mixed siliciclastic-carbonate coast. local geology is significantly...

10.1016/j.sedgeo.2017.06.006 article EN cc-by Sedimentary Geology 2017-06-16

Brown, A.L.; Reinhardt, E.G.; van Hengstum, P.J., and Pilarczyk, J.E., 2014. A coastal Yucatan sinkhole records intense hurricane events.The potential of tropical sinkholes as archives for historical events has yet to be fully explored. This study uses high-resolution (1-cm interval) particle-size analysis examine two sediment push cores from Laguna Chumkopó, located on the Peninsula, Mexico. Core CKC1 (62 cm) was collected base a deep in Chumkopó at −79.9 m (msl), while second core, CKC2...

10.2112/jcoastres-d-13-00069.1 article EN Journal of Coastal Research 2013-12-05

Wave set-up steepened and accentuated the storm surge during Typhoon Haiyan in November 2013 resulting bore-like flooding with heights of 7 m flow velocities reaching 5 s− 1 on open-sea coastal plain near Hernani. This study investigates two distinct sediment assemblages left behind by associated this surge. The first assemblage consists numerous boulders that now occupy reef flat, second pertains to a laterally extensive sand sheet blanketed up ~ 300 inland. majority has b axes between 2 m,...

10.1016/j.margeo.2017.08.016 article EN cc-by-nc-nd Marine Geology 2017-08-26

Research Article| August 01, 2015 Accommodation space, relative sea level, and the archiving of paleo-earthquakes along subduction zones Harvey M. Kelsey; Kelsey 1Department Geology, Humboldt State University, Arcata, California 95524, USA Search for other works by this author on: GSW Google Scholar Simon E. Engelhart; Engelhart 2Department Geosciences, University Rhode Island, Kingston, Island 02881, Jessica Pilarczyk; Pilarczyk 3Department Marine Coastal Science, Rutgers New Brunswick,...

10.1130/g36706.1 article EN Geology 2015-06-23

Abstract Erosional and sedimentary features associated with flooding have been documented in both modern past cases. However, only a few studies demonstrated the relationship between these corresponding hydraulic conditions that produced them, making it difficult to evaluate magnitude of paleo-flooding. This study describes characteristics inundation depth flow direction, as well erosional resulting from disastrous Kinu River, central Japan, September 2015. Water levels rose rapidly due...

10.1038/srep34168 article EN cc-by Scientific Reports 2016-09-28

Abstract Hurricane Irma (September 2017) was one of the most devastating hurricanes in recent times. In January 2018, a post‐hurricane field survey conducted on Anegada (British Virgin Islands) to report erosional and depositional evidence caused by Irma's storm surge waves. We document type extent hurricane‐induced geomorphological changes, allowing for an improved risk assessment hurricane‐related inundation low‐lying islands carbonate platforms. Anegada's north shore impacted Irma. The...

10.1002/esp.5293 article EN cc-by-nc-nd Earth Surface Processes and Landforms 2021-11-27

Abstract Tsunami deposits preserved in the geological record provide a more comprehensive understanding of their patterns frequency and intensity over longer timescales; but recognizing tsunami can prove challenging due to post‐depositional changes, lack contrast between surrounding sedimentary layers, differentiating storm deposition. Modern baseline studies address these challenges by providing insight into modern spatial distributions that be compared with palaeotsunami deposits. This...

10.1111/sed.12591 article EN cc-by Sedimentology 2019-02-19

On September 16, 2015, a Mw 8.3 earthquake struck the north-central Chile coast, triggering tsunami observed along 500 km of coastline, between Huasco (28.5°S) and San Antonio (33.5°S). This provided unique opportunity to examine nature deposits in semi-arid, siliciclastic environment where stratigraphic sedimentological records past tsunamis are difficult distinguish. To improve our ability identify such evidence, we targeted one few low-energy, organic-rich depositional environments Chile:...

10.1016/j.quascirev.2021.107052 article EN cc-by-nc-nd Quaternary Science Reviews 2021-07-21
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