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Publications

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Pollen and spores of terrestrial plants Pollen and spores of terrestrial plants

Pollen and spores are valuable tools in reconstructing past sea level and climate because of their ubiquity, abundance, and durability as well as their reciprocity with source vegetation to environmental change (Cronin, 1999; Traverse, 2007; Willard and Bernhardt, 2011). Pollan is found in many sedimentary environments, from freshwater to saltwater, terrestrial to marine. It can be...
Authors
Christopher E. Bernhardt, Debra A. Willard

Geomorphology, active tectonics, and landscape evolution in the Mid-Atlantic region Geomorphology, active tectonics, and landscape evolution in the Mid-Atlantic region

In 2014, the geomorphology community marked the 125th birthday of one of its most influential papers, “The Rivers and Valleys of Pennsylvania” by William Morris Davis. Inspired by Davis’s work, the Appalachian landscape rapidly became fertile ground for the development and testing of several grand landscape evolution paradigms, culminating with John Hack’s dynamic equilibrium in 1960. As...
Authors
Frank J. Pazzaglia, Mark W. Carter, Claudio Berti, Ronald C. Counts, Gregory S. Hancock, David Harbor, Richard W. Harrison, Matthew J. Heller, Shannon A. Mahan, Helen Malenda, Ryan McKeon, Michelle S. Nelson, Phillip Prince, Tammy M. Rittenour, James Spotilla, G. Richard Whittecar

Quaternary geology of the Boston area: Glacial events from Lake Charles to Lake Aberjona Quaternary geology of the Boston area: Glacial events from Lake Charles to Lake Aberjona

The multiple-glacial and glaciomarine Quaternary history of the Boston, Massachusetts area has been known generally since the earliest studies of the then newly recognized glacial deposits described by Prof. Louis Agassiz in the late1840’s and fossil marine shells in the drift in the 1850’s. Attention then turned to possible glacial erosional effects on the preglacial bedrock...
Authors
Byron D. Stone, John W. Lane

Volcanoes of the passive margin: The youngest magmatic event in eastern North America Volcanoes of the passive margin: The youngest magmatic event in eastern North America

The rifted eastern North American margin (ENAM) provides important clues to the long-term evolution of continental margins. An Eocene volcanic swarm exposed in the Appalachian Valley and Ridge Province of Virginia and West Virginia (USA) contains the youngest known igneous rocks in the ENAM. These magmas provide the only window into the most recent deep processes contributing to the...
Authors
Sarah E Mazza, Esteban Gazel, Elizabeth A Johnson, Michael J. Kunk, Ryan J. McAleer, James A Spotila, Michael Bizimis, Drew S Coleman

Geology and neotectonism in the epicentral area of the 2011 M5.8 Mineral, Virginia, earthquake Geology and neotectonism in the epicentral area of the 2011 M5.8 Mineral, Virginia, earthquake

This fi eld guide covers a two-day west-to-east transect across the epicentral region of the 2011 M5.8 Mineral, Virginia, earthquake, the largest ever recorded in the Central Virginia seismic zone. The fi eld trip highlights results of recent bedrock and surficial geologic mapping in two adjoining 7.5-min quadrangles, the Ferncliff and the Pendleton, which together encompass the...
Authors
William C. Burton, David B. Spears, Richard W. Harrison, Nicholas H. Evans, J. Stephen Schindler, Ronald C. Counts

Stafford fault system: 120 million year fault movement history of northern Virginia Stafford fault system: 120 million year fault movement history of northern Virginia

The Stafford fault system, located in the mid-Atlantic coastal plain of the eastern United States, provides the most complete record of fault movement during the past ~120 m.y. across the Virginia, Washington, District of Columbia (D.C.), and Maryland region, including displacement of Pleistocene terrace gravels. The Stafford fault system is close to and aligned with the Piedmont...
Authors
David S. Powars, Rufus D. Catchings, J. Wright Horton, J. Stephen Schindler, Milan J. Pavich

Neoproterozoic–Cambrian stratigraphic framework of the Anti-Atlas and Ouzellagh promontory (High Atlas), Morocco Neoproterozoic–Cambrian stratigraphic framework of the Anti-Atlas and Ouzellagh promontory (High Atlas), Morocco

In the last two decades, great progress has been made in the geochronological, chrono- and chemostratigraphic control of the Neoproterozoic and Cambrian from the Anti-Atlas Ranges and the Ouzellagh promontory (High Atlas). As a result, the Neoproterozoic is lithostratigraphically subdivided into: (i) the Lkest-Taghdout Group (broadly interpreted at c. 800–690 Ma) representative of rift...
Authors
Jose Javier Alvaro, Fouad Benziane, Robert Thomas, Gregory J. Walsh, Abdelaziz Yazidi

Digital Mapping Techniques '11–12 workshop proceedings Digital Mapping Techniques '11–12 workshop proceedings

The Digital Mapping Techniques '11 (DMT'11) workshop was hosted by Virginia Division of Geology and Mineral Resources and The College of William & Mary, and coordinated by the National Geologic Map Database project. Conducted May 22-25 on the campus of The College of William & Mary, in Williamsburg, Virginia, it was attended by 77 technical experts from 30 agencies, universities, and...
Authors
David R. Soller

Estimates of natural salinity and hydrology in a subtropical estuarine ecosystem: implications for Greater Everglades restoration Estimates of natural salinity and hydrology in a subtropical estuarine ecosystem: implications for Greater Everglades restoration

Disruption of the natural patterns of freshwater flow into estuarine ecosystems occurred in many locations around the world beginning in the twentieth century. To effectively restore these systems, establishing a pre-alteration perspective allows managers to develop science-based restoration targets for salinity and hydrology. This paper describes a process to develop targets based on...
Authors
Frank E. Marshall, G. Lynn Wingard, Patrick A. Pitts

A sub-national scale geospatial analysis of diamond deposit lootability: the case of the Central African Republic A sub-national scale geospatial analysis of diamond deposit lootability: the case of the Central African Republic

The Central African Republic (CAR), a country with rich diamond deposits and a tumultuous political history, experienced a government takeover by the Seleka rebel coalition in 2013. It is within this context that we developed and implemented a geospatial approach for assessing the lootability of high value-to-weight resource deposits, using the case of diamonds in CAR as an example...
Authors
Katherine C. Malpeli, Peter G. Chirico

Late Holocene sea- and land-level change on the U.S. southeastern Atlantic Coast Late Holocene sea- and land-level change on the U.S. southeastern Atlantic Coast

Late Holocene relative sea-level (RSL) reconstructions can be used to estimate rates of land-level (subsidence or uplift) change and therefore to modify global sea-level projections for regional conditions. These reconstructions also provide the long-term benchmark against which modern trends are compared and an opportunity to understand the response of sea level to past climate...
Authors
Andrew C. Kemp, Christopher E. Bernhardt, Benjamin P. Horton, Robert E. Kopp, Christopher H. Vane, W. Richard Peltier, Andrea D. Hawkes, Jeffrey P. Donnelly, Andrew C. Parnell, Niamh Cahill

Catinaster virginianus sp. nov.: A new species of Catinaster from the middle Miocene Mid-Atlantic Coastal Plain Catinaster virginianus sp. nov.: A new species of Catinaster from the middle Miocene Mid-Atlantic Coastal Plain

High-resolution analysis of sediments from four coreholes associated with the Chesapeake Bay impact crater has resulted in the identification of a new species, Catinaster virginianus. This species is similar to Catinaster coalitus coalitus, but differs in having a proximal stem. The first occurrence of C. virginianus is in Zone NN5, and is older than any previously identified Catinaster...
Authors
Jean M. Self-Trail
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