Publications
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What is the Anthropocene?
Since Paul Crutzen and Eugene Stoermer introduced the word “Anthropocene” in 2000, scientists and nonscientists alike have used the word to highlight the concept that we are now living in a time when the global environment, at some level, is shaped by humankind rather than vice versa. Humans have significantly altered Earth’s land surface, oceans, rivers, atmosphere, flora, and fauna. By its emph
Authors
Lucy E. Edwards
Topographic and Hydrographic GIS Datasets for the Afghanistan Geological Survey and U.S. Geological Survey 2014 Mineral Areas of Interest
Mineral extraction and associated industries play an important role in the Afghan economy, particularly in the “transitional era” of declining foreign aid and withdrawal of foreign troops post 2014. In addition to providing a substantial source of government revenue, other potential benefits of natural resource development include boosted exports, employment opportunities, and strengthened industr
Authors
Jessica D. DeWitt, Peter G. Chirico, Katherine C. Malpeli
Karst mapping in the United States: Past, present and future
The earliest known comprehensive karst map of the entire USA was published by Stringfield and LeGrand (1969), based on compilations of William E. Davies of the U.S. Geological Survey (USGS). Various versions of essentially the same map have been published since. The USGS recently published new digital maps and databases depicting the extent of known karst, potential karst, and pseudokarst areas of
Authors
David J. Weary, Daniel H. Doctor
Geochemistry and origin of metamorphosed mafic rocks from the Lower Paleozoic Moretown and Cram Hill Formations of North-Central Vermont: Delamination magmatism in the western New England appalachians
The Moretown Formation, exposed as a north-trending unit that extends from northern Vermont to Connecticut, is located along a critical Appalachian litho-tectonic zone between the paleomargin of Laurentia and accreted oceanic terranes. Remnants of magmatic activity, in part preserved as metamorphosed mafic rocks in the Moretown Formation and the overlying Cram Hill Formation, are a key to further
Authors
Raymond Coish, Jonathan Kim, Evan Twelker, Scott P. Zolkos, Gregory J. Walsh
The Chesapeake Bay impact structure
About 35 million years ago, during late Eocene time, a 2-mile-wide asteroid or comet smashed into Earth in what is now the lower Chesapeake Bay in Virginia. The oceanic impact vaporized, melted, fractured, and (or) displaced the target rocks and sediments and sent billions of tons of water, sediments, and rocks into the air. Glassy particles of solidified melt rock rained down as far away as Texas
Authors
David S. Powars, Lucy E. Edwards, Gregory S. Gohn, J. Wright Horton
Chesapeake Bay impact structure: A blast from the past
About 35 million years ago, a 2-mile-wide meteorite smashed into Earth in what is now the lower Chesapeake Bay in Virginia. The oceanic impact vaporized, melted, fractured, and displaced rocks and sediments and sent billions of tons of water, sediments, and rocks into the air. Glassy particles of solidified melt rock rained down as far away as Texas and the Caribbean. Large tsunamis affected most
Authors
David S. Powars, Lucy E. Edwards, Gregory S. Gohn, J. Wright Horton
Geologic map of Kundelan ore deposits and prospects, Zabul Province, Afghanistan; modified from the 1971 original map compilations of K.I. Litvinenko and others
This map and cross sections are redrafted modified versions of the Geological map of the Kundelan ore deposit area, scale 1:10,000 (graphical supplement no. 18) and the Geological map of the Kundelan deposits, scale 1:2,000 (graphical supplement no. 3) both contained in an unpublished Soviet report by Litvinenko and others (1971) (report no. 0540). The unpublished Soviet report was prepared in coo
Authors
Robert D. Tucker, Stephen G. Peters, Will R. Stettner, Linda M. Masonic, Thomas W. Moran
On the reconstruction of palaeo-ice sheets: Recent advances and future challenges
Reconstructing the growth and decay of palaeo-ice sheets is critical to understanding mechanisms of global climate change and associated sea-level fluctuations in the past, present and future. The significance of palaeo-ice sheets is further underlined by the broad range of disciplines concerned with reconstructing their behaviour, many of which have undergone a rapid expansion since the 1980s. In
Authors
Chris R. Stokes, Lev Tarasov, Robin Blomdin, Thomas M. Cronin, Timothy G. Fisher, Richard Gyllencreutz, Clas Hattestrand, Jakob Heyman, Richard C. A. Hindmarsh, Anna L. C. Hughes, Martin Jakobsson, Nina Kirchner, Stephen J. Livingstone, Martin Margold, Julian B. Murton, Riko Noormets, W. Richard Peltier, Dorothy M. Peteet, David J. W. Piper, Frank Preusser, Hans Renssen, David H. Roberts, Didier M. Roche, Francky Saint-Ange, Arjen P. Stroeven, James T. Teller
Accommodation space, relative sea level, and the archiving of paleo-earthquakes along subduction zones
The spatial variability of Holocene relative sea-level (RSL) change influences the capacities of coastal environments to accommodate a sedimentary record of paleoenvironmental change. In this study we couch a specific investigation in more general terms in order to demonstrate the applicability of the relative sea-level history approach to paleoseismic investigations. Using subsidence stratigraphy
Authors
Harvey M. Kelsey, Simon E. Engelhart, Jessica E. Pilarczyk, Benjamin P. Horton, Charles Rubin, Mudrik Daryono, Nazli Ismail, Andrea D. Hawkes, Christopher E. Bernhardt, Niamh Cahill
Volcanic ash hazards and aviation risk: Chapter 4
The risks to safe and efficient air travel from volcanic-ash hazards are well documented and widely recognized. Under the aegis of the International Civil Aviation Organization, globally coordinated mitigation procedures are in place to report explosive eruptions, detect airborne ash clouds and forecast their expected movement, and issue specialized messages to warn aircraft away from hazardous ai
Authors
Marianne C. Guffanti, Andrew C. Tupper
The geology of Burnsville Cove, Bath and Highland Counties, Virginia
Burnsville Cove is a karst region in Bath and Highland Counties of Virginia. A new geologic map of the area reveals various units of limestone, sandstone, and siliciclastic mudstone (shale) of Silurian through Devonian age, as well as structural features such as northeast-trending anticlines and synclines, minor thrust faults, and prominent joints. Quaternary features include erosional (strath) te
Authors
Christopher S. Swezey, John T. Haynes, Richard A. Lambert, William B. White, Philip C. Lucas, Christopher P. Garrity
NACSN, note 67--Application for revision of Articles 36 and 37, Lithodemic units of the North American stratigraphic code
Currently the North American Stratigraphic Code, (NACSN 2005, Article 37) sets restrictions on the use of the term “complex” for lithodemic units. With exceptions for “volcanic complex” and “structural complex,” a complex must consist of more than one genetic class of rock (i.e., sedimentary, igneous or metamorphic). Thus, the use of the term “complex” to describe masses of intrusive rocks is not
Authors
Robert M. Easton, Lucy E. Edwards, Randall C. Orndorff, Manuel Duguet, Ismael Ferrusquia-Villafranca