Publications
Scientific reports, journal articles, and information products produced by USGS Pacific Coastal and Marine Science Center scientists.
Filter Total Items: 1453
The tail of the Storegga Slide: Insights from the geochemistry and sedimentology of the Norwegian Basin deposits The tail of the Storegga Slide: Insights from the geochemistry and sedimentology of the Norwegian Basin deposits
Deposits within the floor of the Norwegian Basin were sampled to characterize the deposition from the Storegga Slide, the largest known Holocene-aged continental margin slope failure complex. A 29 to 67 cm thick veneer of variable-coloured, finely layered Holocene sediment caps a homogeneous, extremely well-sorted, poorly consolidated, very fine-grained, grey-coloured sediment section...
Authors
C. K. Paull, W. Ussler, W.S. Holbrook, T.M. Hill, H. Haflidason, W. Winters, T. Lorenson, I. Aiello, J.E. Johnson, E. Lundsten
Carbonate control of H2 and CH4 production in serpentinization systems at elevated P-Ts Carbonate control of H2 and CH4 production in serpentinization systems at elevated P-Ts
Serpentinization of forsteritic olivine results in the inorganic synthesis of molecular hydrogen (H2) in ultramafic hydrothermal systems (e.g., mid-ocean ridge and forearc environments). Inorganic carbon in those hydrothermal systems may react with H2 to produce methane (CH4) and other hydrocarbons or react with dissolved metal ions to form carbonate minerals. Here, we report...
Authors
L. Camille Jones, Robert Rosenbauer, Jonas I. Goldsmith, Christopher Oze
Distribution and tsunamigenic potential of submarine landslides in the Gulf of Mexico Distribution and tsunamigenic potential of submarine landslides in the Gulf of Mexico
The Gulf of Mexico (GOM) is a geologically diverse ocean basin that includes three distinct geologic provinces: a carbonate province, a salt province, and canyon to deep-sea fan province, all of which contain evidence of submarine mass movements. The threat of submarine landslides in the GOM as a generator of near-field damaging tsunamis has not been widely addressed. Submarine...
Authors
Jason D. Chaytor, David C. Twichell, Patrick Lynett, Eric L. Geist
Large-scale coastal change in the Columbia River littoral cell: an overview Large-scale coastal change in the Columbia River littoral cell: an overview
This overview introduces large-scale coastal change in the Columbia River littoral cell (CRLC). Covering 165 km of the southwest Washington and northwest Oregon coasts, the littoral cell is made up of wide low-sloping dissipative beaches, broad coastal dunes and barrier plains, three large estuaries, and is bounded by rocky headlands. The beaches and inner shelf are composed of fine...
Authors
Guy Gelfenbaum, George M. Kaminsky
Seasonal and decadal-scale channel evolution on the dammed Elwha River, Washington Seasonal and decadal-scale channel evolution on the dammed Elwha River, Washington
More than 75,000 dams exist in the continental United States to provide water storage, flood control, and hydropower generation (Graf, 1999). Many of these were built during the early twentieth century and are due for relicensing consideration now and in the near future. The cost of repairing aging dams, together with growing understanding of the ecologic effects of river regulation...
Authors
Amy E. Draut, Joshua B. Logan, Mark C. Mastin, Randall E. McCoy
Estimating the empirical probability of submarine landslide occurrence Estimating the empirical probability of submarine landslide occurrence
The empirical probability for the occurrence of submarine landslides at a given location can be estimated from age dates of past landslides. In this study, tools developed to estimate earthquake probability from paleoseismic horizons are adapted to estimate submarine landslide probability. In both types of estimates, one has to account for the uncertainty associated with age-dating...
Authors
Eric L. Geist, Thomas E. Parsons
Wind-enhanced resuspension in the shallow waters of South San Francisco Bay: Mechanisms and potential implications for cohesive sediment transport Wind-enhanced resuspension in the shallow waters of South San Francisco Bay: Mechanisms and potential implications for cohesive sediment transport
We investigated the driving forces of sediment dynamics at the shoals in South San Francisco Bay. Two stations were deployed along a line perpendicular to a 14 m deep channel, 1000 and 2000 m from the middle of the channel. Station depths were 2.59 and 2.19 m below mean lower low water, respectively. We used acoustic Doppler velocimeters for the simultaneous determination of current...
Authors
Andreas Brand, Jessica R. Lacy, Kevin Hsu, Daniel Hoover, Steve Gladding, Mark T. Stacey
Biogeochemical processes in an urban, restored wetland of San Francisco Bay, California, 2007-2009: Methods and data for plant, sediment and water parameters Biogeochemical processes in an urban, restored wetland of San Francisco Bay, California, 2007-2009: Methods and data for plant, sediment and water parameters
The restoration of 18 acres of historic tidal marsh at Crissy Field has had great success in terms of public outreach and visibility, but less success in terms of revegetated marsh sustainability. Native cordgrass (Spartina foliosa) has experienced dieback and has failed to recolonize following extended flooding events during unintended periodic closures of its inlet channel, which...
Authors
Lisamarie Windham-Myers, Mark C. Marvin-DiPasquale, Jennifer L. Agee, Le H. Kieu, Evangelos Kakouros, Li H. Erikson, Kristen Ward
Anthropogenic influence on recent bathymetric change in west-central San Francisco Bay Anthropogenic influence on recent bathymetric change in west-central San Francisco Bay
Two multibeam sonar surveys of west-central San Francisco Bay, California, were conducted in 1997 and 2008. Bathymetric change analysis between the two surveys indicates a loss of 14.1 million cubic meters (-3.1 cm/yr) of sediment during this time period, representing an approximately three-fold acceleration of the rate that was observed from prior depth change analysis from 1947 to 1979...
Authors
Patrick L. Barnard, Rikk G. Kvitek
An approach for modeling sediment budgets in supply-limited rivers An approach for modeling sediment budgets in supply-limited rivers
Reliable predictions of sediment transport and river morphology in response to variations in natural and human-induced drivers are necessary for river engineering and management. Because engineering and management applications may span a wide range of space and time scales, a broad spectrum of modeling approaches has been developed, ranging from suspended-sediment "rating curves" to...
Authors
Scott Wright, David J. Topping, David M. Rubin, Theodore S. Melis
Dramatic beach and nearshore morphological changes due to extreme flooding at a wave-dominated river mouth Dramatic beach and nearshore morphological changes due to extreme flooding at a wave-dominated river mouth
Record flooding on the Santa Clara River of California (USA) during January 2005 injected ∼ 5 million m3 of littoral-grade sediment into the Santa Barbara Littoral Cell, approximately an order of magnitude more than both the average annual river loads and the average annual alongshore littoral transport in this portion of the cell. This event appears to be the largest sediment transport...
Authors
P.L. Barnard, J.A. Warrick
Spotlight 6: Davidson seamount Spotlight 6: Davidson seamount
Davidson Seamount is located about 80 km off the central California coast in the Monterey Bay National Marine Sanctuary. It is one of the better-explored seamounts in the world, having been sampled and observed during 32 dives by the remotely operated vehicle (ROV) Tiburon. These dives mapped the bottom substrate and biological communities, and collected over 280 rock samples and nearly...
Authors
David A. Clague, L. Lundsten, James R. Hein, Jennifer B. Paduan, Alice Davis