Steven Carey

ORCID: 0009-0001-4846-8919
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About
Contact & Profiles
Research Areas
  • earthquake and tectonic studies
  • Geological and Geochemical Analysis
  • Geology and Paleoclimatology Research
  • Methane Hydrates and Related Phenomena
  • Geological formations and processes
  • Geological and Tectonic Studies in Latin America
  • High-pressure geophysics and materials
  • Radio Astronomy Observations and Technology
  • Drilling and Well Engineering
  • Reservoir Engineering and Simulation Methods
  • Offshore Engineering and Technologies
  • Geological and Geophysical Studies
  • Ocean Acidification Effects and Responses
  • Geochemistry and Geologic Mapping
  • Meteorological Phenomena and Simulations
  • Astrophysics and Cosmic Phenomena
  • Antenna Design and Optimization
  • Oceanographic and Atmospheric Processes
  • Maritime and Coastal Archaeology
  • Geological and Geophysical Studies Worldwide
  • Seismic Waves and Analysis
  • Paleontology and Stratigraphy of Fossils
  • Marine and environmental studies
  • Mineralogy and Gemology Studies
  • Millimeter-Wave Propagation and Modeling

University of Cambridge
2024-2025

University of Rhode Island
2009-2023

Ohio University
2023

Oceanography Society
2016

Maine Department of Marine Resources
2016

The Mount St. Helens, May 18 pumice is a dacite containing 60% glass by weight and phenocrysts of plagioclase, orthopyroxene, amphibole, titaniferous magnetite, ilmenite. uniform in composition, rhyodacite with 73 wt % SiO 2 ; the are also composition except for which has cores averaging An 57 rims 49 . Analyses seven pairs coexisting Fe‐Ti oxides representative sample light were recast using various mineral calculation procedures; they yielded temperatures ranging from 920° to 940°C ‐log ƒ...

10.1029/jb090ib04p02929 article EN Journal of Geophysical Research Atmospheres 1985-03-10

Abstract On Dec. 22, 2018, at approximately 20:55–57 local time, Anak Krakatau volcano, located in the Sunda Straits of Indonesia, experienced a major lateral collapse during period eruptive activity that began June. The discharged volcaniclastic material into 250 m deep caldera southwest which generated tsunami with runups up to 13 on adjacent coasts Sumatra and Java. caused least 437 fatalities, greatest number from volcanically-induced since catastrophic explosive eruption 1883 sector...

10.1038/s41598-019-48327-6 article EN cc-by Scientific Reports 2019-08-16

Cetyltrimethylammonium bromide (CTAB)-based methods are widely used to isolate DNA from plant tissues, but the unique chemical composition of secondary metabolites among species has necessitated optimization. Research articles often cite a "modified" CTAB protocol without explicitly stating how had been altered, creating non-reproducible studies. Furthermore, various modifications that have applied not rigorously reviewed and doing so could reveal optimization strategies across study...

10.1002/aps3.11517 article EN cc-by Applications in Plant Sciences 2023-05-01

10.1007/bf01086759 article EN Bulletin of Volcanology 1989-01-01

Research Article| August 01, 1987 Temporal variations in column height and magma discharge rate during the 79 A.D. eruption of Vesuvius STEVEN CAREY; CAREY 1Graduate School Oceanography, University Rhode Island, Kingston, Island 02881 Search for other works by this author on: GSW Google Scholar HARALDUR SIGURDSSON GSA Bulletin (1987) 99 (2): 303–314. https://doi.org/10.1130/0016-7606(1987)99<303:TVICHA>2.0.CO;2 Article history first online: 01 Jun 2017 Cite View This Citation Add to Manager...

10.1130/0016-7606(1987)99<303:tvicha>2.0.co;2 article EN Geological Society of America Bulletin 1987-01-01

The most recent major explosive eruption of the Santorini volcano in Greece—around 3600 years before present (B.P.), often referred to as Minoan eruption—is one largest volcanic events known historical time and has been subject intense volcanological archeological studies [ Druitt et al ., 1999]. submarine Kolumbo, located seven kilometers northeast associated with Santorini's tectonic system, erupted explosively 1650 A.D., resulting fatalities on island Thera Fouqué , 1879]. A large...

10.1029/2006eo340001 article EN Eos 2006-08-22

We report on integrated geomorphological, mineralogical, geochemical and biological investigations of the hydrothermal vent field located floor density-stratified acidic (pH ~ 5) crater Kolumbo shallow-submarine arc-volcano, near Santorini. features rare geodynamic setting at convergent boundaries, where arc-volcanism seafloor activity are occurring in thinned continental crust. Special focus is given to unique enrichments polymetallic spires Sb Tl (±Hg, As, Au, Ag, Zn) indicating a new...

10.1038/srep02421 article EN cc-by-nc-sa Scientific Reports 2013-08-13

Despite their global societal importance, the volumes of large-scale volcanic eruptions remain poorly constrained. Here, we integrate seismic reflection and P-wave tomography datasets with computed tomography-derived sedimentological analyses to estimate volume iconic Minoan eruption. Our results reveal a total dense-rock equivalent eruption 34.5 ± 6.8 km³, which encompasses 21.4 3.6 km³ tephra fall deposits, 6.9 2 ignimbrites, 6.1 1.2 intra-caldera deposits. 2.8 1.5 material consists...

10.1038/s41467-023-38176-3 article EN cc-by Nature Communications 2023-04-29

Abstract This paper presents the design and deployment of Hydrogen Epoch Reionization Array (HERA) phase II system. HERA is designed as a staged experiment targeting 21 cm emission measurements Reionization. First results from I array are published early 2022, system nearing completion. We describe discuss progress on commissioning future upgrades. As designated Square Kilometre pathfinder instrument, we also show number “case studies” that investigate systematics seen while system, which...

10.1088/1538-3873/ad3122 article EN cc-by Publications of the Astronomical Society of the Pacific 2024-04-01

Research Article| September 01, 1997 Influence of convective sedimentation on the formation widespread tephra fall layers in deep sea Steven Carey 1Graduate School Oceanography, University Rhode Island, South Ferry Road, Narragansett, Island 02882 Search for other works by this author on: GSW Google Scholar Author and Article Information Publisher: Geological Society America First Online: 02 Jun 2017 Online ISSN: 1943-2682 Print 0091-7613 Geology (1997) 25 (9): 839–842....

10.1130/0091-7613(1997)025<0839:iocsot>2.3.co;2 article EN Geology 1997-01-01

10.1016/0377-0273(83)90063-x article EN Journal of Volcanology and Geothermal Research 1983-09-01

The Plinian phase of the May 18, 1980, Mount St. Helens eruption is modeled as a steady state discharge dacitic magma from reservoir at 7–10 km depth rate 1.94×10 7 kg/s. Properties magma, including preeruption volatile content (4.6% in melt), temperature (920°–940° C), and confining pressure (190–250 MPa) are constrained by petrologic studies. Mass rate, viscosity, independent estimates ascent velocity suggest 95‐m‐diameter conduit below vapor saturation. Dispersal pyroclasts indicate...

10.1029/jb090ib04p02948 article EN Journal of Geophysical Research Atmospheres 1985-03-10

Summary Marginal basins adjacent to oceanic island arcs receive volcaniclastic debris from the bordering volcanic arc, back-arc spreading centre, and, a lesser degree, remnant arc. The arc is volumetrically most important source, with abundant volcaniclastics being produced by explosive subaerial and/or subaqueous eruptions and secondary erosion of complex. Transport material deeper parts marginal occurs passive settling through water column or variety sediment gravity flows generated...

10.1144/gsl.sp.1984.016.01.04 article EN Geological Society London Special Publications 1984-01-01

Abstract Caldera-forming eruptions of island volcanoes generate tsunamis by the interaction different eruptive phenomena with sea. Such are a major hazard, but forward models their impacts limited poor understanding source mechanisms. The caldera-forming eruption Santorini in Late Bronze Age is known to have been tsunamigenic, and caldera collapse has proposed as mechanism. Here, we present bathymetric seismic evidence showing that was not open sea during main phase eruption, flooded once...

10.1038/ncomms13332 article EN cc-by Nature Communications 2016-11-08

Research Article| September 01, 2013 CO2 degassing from hydrothermal vents at Kolumbo submarine volcano, Greece, and the accumulation of acidic crater water Steven Carey; Carey 1Graduate School Oceanography, University Rhode Island, 215 S. Ferry Road, Narragansett, Island 02882, USA Search for other works by this author on: GSW Google Scholar Paraskevi Nomikou; Nomikou 2Faculty Geology Geoenvironment, Athens, Zografou, 157 84 Greece Katy Croff Bell; Bell Marvin Lilley; Lilley 3School...

10.1130/g34286.1 article EN Geology 2013-07-12

The Late Bronze Age ‘Minoan’ eruption of Santorini, Greece occurred from within an existing caldera. Low-temperature pyroclastic flow emplacement on shallow slopes outside the caldera can only be consistent with being filled products that are not preserved. Field observations and seismic reflection surveys suggest this missing material has been downfaulted. volume infill is estimated as 18–26 km 3 dense rock equivalent (DRE), increasing total Minoan deposits to 78–86 DRE making it largest...

10.1144/jgs2013-113 article EN Journal of the Geological Society 2014-06-09

Abstract This study reports the first detailed geochemical characterization of Kolumbo submarine volcano in order to investigate role source heterogeneity controlling variability within Santorini volcanic field central Aegean arc. Kolumbo, situated 15 km northeast Santorini, last erupted 1650 AD and is thus closely associated with system space time. Samples taken by remotely‐operated vehicle that were analyzed for major element, trace element Sr‐Nd‐Hf‐Pb isotope composition include...

10.1002/2016gc006398 article EN cc-by-nc-nd Geochemistry Geophysics Geosystems 2016-07-11
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