John E. Sanders

ORCID: 0000-0003-4071-2099
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About
Contact & Profiles
Research Areas
  • Geological formations and processes
  • Geology and Paleoclimatology Research
  • Coastal and Marine Dynamics
  • Geological Modeling and Analysis
  • Paleontology and Stratigraphy of Fossils
  • Geological and Geochemical Analysis
  • Coastal wetland ecosystem dynamics
  • Atmospheric chemistry and aerosols
  • Aeolian processes and effects
  • Atmospheric Ozone and Climate
  • Hydrology and Sediment Transport Processes
  • Atmospheric and Environmental Gas Dynamics
  • Geochemistry and Geologic Mapping
  • Botany, Ecology, and Taxonomy Studies
  • Geological Studies and Exploration
  • Landslides and related hazards
  • Marine Biology and Ecology Research
  • Archaeology and Natural History
  • Fire effects on ecosystems
  • Underwater Acoustics Research
  • Marine and coastal plant biology
  • Water Quality and Resources Studies
  • Species Distribution and Climate Change
  • Urban Green Space and Health
  • Tree-ring climate responses

University of California, Berkeley
2015-2020

University of Miami
2011-2014

Hofstra University
1996-1997

City University of New York
1996

Barnard College
1970-1983

Columbia University
1970-1982

Lamont-Doherty Earth Observatory
1974

Rensselaer Polytechnic Institute
1969-1970

Hudson Institute
1966-1969

Yale University
1957-1962

This book has been written in response to the rapid expansion and diversification of sedimentology during last 30 years. We believe that a critical synthesis this field is matter importance urgency. The study involves dynamic interplay with many other branches geology. Its tools range from those used measure submicroscopic ones involving use radar, reflection seismograph, Earth satellites. In introduction Part I we define wide scope sedimentology, as see it, which may be broader than some...

10.2307/632883 article EN Geographical Journal 1980-07-01

ABSTRACT Cores of shoreface sediments off Fire Island, Long New York, in water depths ranging between 5 and 21 m, contain a distinctive three-part sequence; from base upward consisting of: (a) basal lag, up to 50 cm thick, containing coarse gravel; (b) finely laminated sand 2 m having median diameters 0.210 0.125 ram, (c) burrow-mottled coarser size than unit (b), 30 thick. The boundaries (a), are sharp. relatively coarser, mottled composing the upper part this sequence results processes...

10.1306/212f6edd-2b24-11d7-8648000102c1865d article EN Journal of Sedimentary Research 1976-01-01

ABSTRACT Tidal inlets, narrow, comparatively deep gaps between barrier islands, are channels through which tidal currents flow vigorously as the water enters and leaves backbarrier lagoons, bays, intertidal flats marshes. Many geologists have compared inlets to river speculated that if an inlet shifts laterally, it should deposit a distinctive sequence of sediments, analogous point‐bar left by meandering stream channel. Fire Island Inlet, located 56 km east New York City, has migrated WSW at...

10.1111/j.1365-3091.1974.tb01788.x article EN Sedimentology 1974-11-01

Research Article| January 01, 1975 Evidence of Shoreface Retreat and In-Place "Drowning" During Holocene Submergence Barriers, Shelf off Fire Island, New York JOHN E. SANDERS; SANDERS 1Department Geology, Barnard College, Columbia University, York, 10027 Search for other works by this author on: GSW Google Scholar NARESH KUMAR 2Department 100273Present address: Lamont-Doherty Geological Observatory at Palisades, 10964. Author Article Information Publisher: Society America First Online: 01...

10.1130/0016-7606(1975)86<65:eosrai>2.0.co;2 article EN Geological Society of America Bulletin 1975-01-01

Abstract. The San Joaquin Valley (SJV) experiences some of the worst ozone air quality in US, frequently exceeding California 8 h standard 70.4 ppb. To improve our understanding trends number violations SJV, we analyze observed relationships between organic reactivity, nitrogen oxides (NOx), and daily maximum temperature southern SJV using measurements made as part at Nexus Air Quality Climate Change 2010 (CalNex-SJV). We find daytime speciated reactivity with respect to OH during CalNex-SJV...

10.5194/acp-14-3373-2014 article EN cc-by Atmospheric chemistry and physics 2014-04-04

ABSTRACT The Holocene history of south-central Long-Island and the adjacent inner continental shelf, as recorded in stratigraphy transgressive deposits, was studied, using information obtained from more than 400 boreholes, cores, marsh probings barrier- backbarrier-areas vibracores numerous seismic-reflection bathymetric profiles on shelf. A sequence deposits which records Flandrian transgression is preserved backbarrier areas Long Island. vertical these trangressive produced by movement...

10.1306/212f7b7b-2b24-11d7-8648000102c1865d article EN Journal of Sedimentary Research 1980-01-01

Abstract. A relaxed eddy accumulation (REA) system combined with a nitrous acid (HONO) analyzer was developed to measure atmospheric HONO vertical fluxes. The consists of three major components: (1) fast-response sonic anemometer measuring both wind velocity and air temperature, (2) controlling unit separating motions into updraft downdraft samplers by the sign velocity, (3) highly sensitive based on aqueous long path absorption photometry that measures concentrations in updrafts downdrafts....

10.5194/amt-4-2093-2011 article EN cc-by Atmospheric measurement techniques 2011-10-07

Abstract Measurements of HONO (g) and particulate nitrite (NO 2 − (p) ) were made with a modified Ambient Ion Monitor–Ion Chromatography (AIM‐IC) instrument during California at the Nexus Air Quality Climate 2010 in Bakersfield, CA (CalNex‐San Joaquin Valley (SJV)). Observations gas matter (PM 2.5 water‐soluble composition showed accumulation both species night, followed by loss next day. Intercomparison Stripping Coil‐UV/Vis Absorption Photometer (SC‐AP) demonstrated excellent agreement...

10.1002/2013jd020971 article EN Journal of Geophysical Research Atmospheres 2014-06-10

The Upper Triassic rocks of the New York-New Jersey-Pennsylvania and Connecticut Valley belts, generally considered to be deposits isolated basins, are inferred represent remnants filling an elongate rift valley that was 50 70 mi wide. In addition, stratigraphic thickness is hold approximately 30,000 ft. If these 2 conclusions correct, then Late tectonic history considerably more complex than previously thought can subdivided into 4 episodes. Episode 1: Initial graben subsidence without...

10.2475/ajs.261.6.501 article EN American Journal of Science 1963-06-01

Research Article| November 01, 1957 CORRELATION OF THE TRIASSIC FORMATIONS NORTH AMERICA EXCLUSIVE CANADA JOHN B REESIDE, JR. (Chairman); (Chairman) U. S. GEOLOGICAL SURVEY, WASHINGTON 25, D. C. Search for other works by this author on: GSW Google Scholar P. L APPLIN; APPLIN E. H COLBERT; COLBERT J. T GREGORY; GREGORY H. D HADLEY; HADLEY BERNHARD KUMMEL; KUMMEL J LEWIS; LEWIS LOVE; LOVE MANUEL MALDONADO-KOERDELL; MALDONADO-KOERDELL MCKEE; MCKEE MCLAUGHLIN; MCLAUGHLIN W MULLER; MULLER A...

10.1130/0016-7606(1957)68[1451:cottfo]2.0.co;2 article EN Geological Society of America Bulletin 1957-01-01

ABSTRACT Three lines of evidence based on data from more than 400 boreholes and vibrocores have been used to reconstruct the evolution barrier islands during Holocene transgression in southern Long Island, New York: (1) transgressive stratigraphic sequence behind present barriers, (2) patterns inner shelf, (3) morphology now‐buried late Pleistocene coastal features. The extensive preservation backbarrier sediments, radiocarbon dated between 7000 8000 yr BP, shelf Island suggests that...

10.1111/j.1365-3091.1981.tb01661.x article EN Sedimentology 1981-02-01

Abstract Comparison of streaked-out “ripples” formed by the drag effects a current passing over watery, yet cohesive sediment bottom with convoluted laminae within beds fine-grained sandstone suggests common origin. Application Bagnold's recent discoveries on behaviour cohesionless in flowing fluids to problem results modification Kuenen's hypothesis origin convolutions. According new interpretation, convolutions arise when formerly sand grains become after deposition and respond increased...

10.1017/s0016756800061768 article EN Geological Magazine 1960-10-01

Research Article| April 01, 1960 SYMMICTITE: A NAME FOR NONSORTED TERRIGENOUS SEDIMENTARY ROCKS THAT CONTAIN WIDE RANGE OF PARTICLE SIZES R. F FLINT; FLINT YALE UNIVERSITY, NEW HAVEN, CONN. Search for other works by this author on: GSW Google Scholar J. E SANDERS; SANDERS JOHN RODGERS Author and Article Information Publisher: Geological Society of America Received: 12 Nov 1959 First Online: 02 Mar 2017 Online ISSN: 1943-2674 Print 0016-7606 Copyright © 1960, The America, Inc. is not claimed...

10.1130/0016-7606(1960)71[507:sanfnt]2.0.co;2 article EN Geological Society of America Bulletin 1960-04-01

Research Article| February 01, 1982 Time-temperature-burial significance of Devonian anthracite implies former great (∼6.5 km) depth burial Catskill Mountains, New York Gerald M. Friedman; Friedman 1Department Geology, Rensselaer Polytechnic Institute, Troy, 12181 Search for other works by this author on: GSW Google Scholar John E. Sanders 2Department Barnard College, Columbia University, York, 10027 Author and Article Information Publisher: Geological Society America First Online: 01 Jun...

10.1130/0091-7613(1982)10<93:tsodai>2.0.co;2 article EN Geology 1982-01-01

ABSTRACT Micritic envelopes are commonly believed to develop from the lime‐mud infillings of circumferential perforations made in skeletal particles by algae. Because “algae” usually taken mean photosynthetic algae, corollary has been proposed that micritic would not appear on carbonate originating waters too deep for active growth Extensions this “photosynthetic‐algae‐only” origin implies that: ( 1 ) disappearance with depth could mark a useful paleobathymetric datum; and 2 preservation...

10.1111/j.1365-3091.1971.tb00220.x article EN Sedimentology 1971-03-01

"Sedimentary structures and current-direction phenomena of the Kulm (lower Carboniferous) Floezleeres (upper graywackes eastern Rhenish Schiefergebirge (Sauerland) Oberharz areas, central Germany, have been examined in reconnaissance. These rocks are interpreted as deposits made by turbidity currents a relatively deep marine trough whose deepest portion migrated slowly northwestward across geosynclinal tract."

10.2475/ajs.254.11.649 article EN American Journal of Science 1956-11-01

ABSTRACT The Pleasantview sandstone is a typical Pennsylvanian cyclothem in western Illinois exhibiting both channel and non-channel phases. In order to describe the interpret sediment transport direction environmental conditions existing at time of deposition, an investigation was made texture, composition, depositional structure, cross-bedding, dimensional fabric. Results this study indicate that subgraywacke which deposited north northwest direction. It concluded process cut large degree...

10.1306/74d70655-2b21-11d7-8648000102c1865d article EN Journal of Sedimentary Research 1957-01-01

Research Article| February 01, 1981 Episodic growth of Holocene tidal marshes in the northeastern United States: A possible indicator eustatic sea-level fluctuations Michael R. Rampino; Rampino 1NASA Goddard Institute for Space Studies, Flight Center, New York, York 10025 Search other works by this author on: GSW Google Scholar John E. Sanders 2Department Geology, Barnard College, Columbia University, 10027 Geology (1981) 9 (2): 63–67....

10.1130/0091-7613(1981)9<63:egohtm>2.0.co;2 article EN Geology 1981-01-01

ABSTRACT Primary sedimentary structures can be used to infer conditions of flow which prevailed within fluid currents deposited the sediment. Three particularly important conclusions about drawn from primary structures: 1) The mechanisms suspension and traction, as defined by G. K. Gilbert in 1914, are fundamentally different, recognized different gross they produce sediments, effects brought distinctive paths followed particles move under influence each mechanism; 2) grain-to-grain...

10.1306/74d70df3-2b21-11d7-8648000102c1865d article EN Journal of Sedimentary Research 1963-01-01
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