Sedimentologic characteristics of recent washover deposits from Assateague Island, Maryland

Application of Ground Penetrating Radar for Identification of Washover Deposits and Other Stratigraphic Features: Assateague Island, MD

Journal of Environmental and Engineering Geophysics ◽

10.2113/jeeg21.4.173 ◽

2016 ◽

Vol 21 (4) ◽

pp. 173-186 ◽

Cited By ~ 6

Author(s):

Nicholas J. Zaremba ◽

Christopher G. Smith ◽

Julie C. Bernier ◽

Arnell S. Forde

Keyword(s):

Ground Penetrating Radar ◽

Washover Deposits ◽

Ground Penetrating ◽

Assateague Island

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Raw and processed ground-penetrating radar and postprocessed differential global positioning system data collected from Assateague Island, Maryland, October 2014

Data Series ◽

10.3133/ds989 ◽

2016 ◽

Author(s):

Nicholas J. Zaremba ◽

Julie C. Bernier ◽

Arnell S. Forde ◽

Christopher G. Smith

Keyword(s):

Global Positioning System ◽

Ground Penetrating Radar ◽

Positioning System ◽

Global Positioning ◽

System Data ◽

Ground Penetrating ◽

Assateague Island ◽

Differential Global Positioning System

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USGS, NPS, and NASA investigate horse-grazing impacts on Assateague Island dunes using airborne lidar surveys

Open-File Report ◽

10.3133/ofr01382 ◽

2001 ◽

Cited By ~ 1

Author(s):

Georgia H. Stoppelaire ◽

John Brock ◽

Chris Lea ◽

Mark Duffy ◽

William Krabill

Keyword(s):

Airborne Lidar ◽

Grazing Impacts ◽

Assateague Island

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SPATIAL AND TEMPORAL PATTERNS OF GROUNDWATER ELEVATION AND SALINITY ON ASSATEAGUE ISLAND

10.1130/abs/2016am-283459 ◽

2016 ◽

Author(s):

Ruth Coffey ◽

◽

Hannah Sprinkle ◽

Eric Sherry ◽

Brian Sturgis ◽

...

Keyword(s):

Temporal Patterns ◽

Spatial And Temporal Patterns ◽

Assateague Island

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NON-LINEAR SHORELINE CHANGE MODELING OF THE NORTHERN VIRGINIA COAST: VIRGINIA BARRIER ISLANDS AND ASSATEAGUE ISLAND

10.1130/abs/2017se-291183 ◽

2017 ◽

Author(s):

Michael S. Fenster ◽

◽

Brian Rizzo ◽

John McManus

Keyword(s):

Barrier Islands ◽

Shoreline Change ◽

Non Linear ◽

Assateague Island

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GEOPHYSICAL AND STRATIGRAPHIC INVESTIGATION OF ASSATEAGUE ISLAND, VIRGINIA: UNRAVELING THE EVOLUTION OF THE ONLY MID-ATLANTIC DUPLEXED BARRIER ISLAND SYSTEM

10.1130/abs/2018ne-311182 ◽

2018 ◽

Author(s):

Brandon Sutter ◽

◽

Bojan Milinic ◽

Sarah Moriarty ◽

Adrienne Oakley ◽

...

Keyword(s):

Barrier Island ◽

Island System ◽

Assateague Island

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SPIT ELONGATION AS A CONTROL ON DOWNDRIFT BARRIER-ISLAND STABILITY- INSIGHTS FROM ASSATEAGUE ISLAND, VA

10.1130/abs/2020se-344286 ◽

2020 ◽

Author(s):

Chloe A. Obara ◽

◽

Justin L. Shawler ◽

Jennifer E. Connell ◽

Christopher J. Hein

Keyword(s):

Barrier Island ◽

Assateague Island

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ANALYSIS OF LOBLOLLY PINE (PINUS TAEDA) TREE RING AND CLIMATE RECORDS OF ASSATEAGUE ISLAND AND CHINCOTEAGUE BAY REGION, VIRGINIA

10.1130/abs/2020se-345333 ◽

2020 ◽

Author(s):

Margaret S. Dunkelberger ◽

◽

Sean R. Cornell ◽

Robert T. Joyce

Keyword(s):

Pinus Taeda ◽

Tree Ring ◽

Loblolly Pine ◽

Climate Records ◽

Chincoteague Bay ◽

Assateague Island

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Genesis and Preservation of Antidune Stratification in Modern and Ancient Washover Deposits: ABSTRACT

AAPG Bulletin ◽

10.1306/03b5adb8-16d1-11d7-8645000102c1865d ◽

1983 ◽

Vol 67 ◽

Cited By ~ 1

Author(s):

J. H. Barwis, M. O. Hayes

Keyword(s):

Washover Deposits

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OVERWASH PROCESSES ON ASSATEAGUE ISLAND

Coastal Engineering Proceedings ◽

10.9753/icce.v14.70 ◽

1974 ◽

Vol 1 (14) ◽

pp. 70

Author(s):

John S. Fisher ◽

Stephen P. Leatherman ◽

Frederick C. Perry

Keyword(s):

Barrier Island ◽

Morphological Features ◽

Northern Portion ◽

Sedimentary Dynamics ◽

Assateague Island

The primary barrier dune on the northern portion of Assateague Island, Maryland is presently being scarped on its seaward face and breached by storm-generated surges. During storms, sediment-ladened water moves across the dune line onto the barrier flats as overwash. The objective of this project is to determine the role overwash plays in barrier island sedimentary dynamics. An overwash model has been suggested. The nonvegetated overwash fan serves as a reservoir for the eventual distribution of the storm-deposited sand. Eolian processes, after the storm, determine the net contribution of overwash sand to each of the different morphological features, i.e., dunes, marsh, beach, etc.

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