Skip to main content
U.S. flag

An official website of the United States government

Book Chapters

Browse more than 5,500 book chapters authored by our scientists over the past 100+ year history of the USGS and refine search by topic, location, year, and advanced search.

Filter Total Items: 6173

Carbon flux, storage, and wildlife co-benefits in a restoring estuary Carbon flux, storage, and wildlife co-benefits in a restoring estuary

Tidal marsh restorations may result in transitional mudflat habitats depending on hydrological and geomorphological conditions. Compared to tidal marsh, mudflats are thought to have limited value for carbon sequestration, carbon storage, and foraging benefits for salmon. We evaluated greenhouse gas exchange, sediment carbon storage, and invertebrate production at restoration and...
Authors
Isa Woo, Melanie J. Davis, Susan E.W. De La Cruz, Lisamarie Windham-Myers, Judith Z. Drexler, Kristin B. Byrd, Ellen Stuart-Haëntjens, Frank E Anderson, Brian A. Bergamaschi, Glynnis Nakai, Christopher S. Ellings, Sayre Hodgson

Ecosystem service co-benefits provided through wetland carbon management Ecosystem service co-benefits provided through wetland carbon management

What is the role of wetland carbon management in providing ecosystem services? Ecosystem services are the benefits that nature provides to people, and they are often categorized as: provisioning (e.g., food and water), regulating (e.g., climate mitigation and flood protection), cultural (e.g., cultural and recreational), and supporting (e.g., nutrient cycling) services ( www...
Authors
Emily Pindilli

Land management strategies influence soil organic carbon stocks of prairie potholes of North America Land management strategies influence soil organic carbon stocks of prairie potholes of North America

Soil organic carbon (SOC) stocks of Prairie Pothole Region (PPR) wetlands in the central plains of Canada and the United States are highly variable due to natural variation in biota, soils, climate, hydrology, and topography. Land-use history (cropland, grassland) and land-management practices (drainage, restoration) also affect SOC stocks. We conducted a region-wide assessment of...
Authors
Sheel Bansal, Brian Tangen, Robert A. Gleason, Pascal Badiou, Irena F. Creed

Data services in ocean science with a focus on the biology Data services in ocean science with a focus on the biology

Biological ocean science has a long history; it goes back millennia, whereas the related data services have emerged in the recent digital era of the past decades. To understand where we come from—and why data services are so important—we will start by taking you back to the rise in the study of marine biology—marine biodiversity—and its key players, before immersing ourselves in the data...
Authors
Joana Beja, Leen Vandepitte, Abigail Benson, Anton Van de Putte, Dan Lear, Daphnis De Pooter, Gwenaelle Moncoiffe, John Nicholls, Nina Wambiji, Patricia Miloslavich, Vasilis Gerovasileiou

Fire and forests in the 21st century: Managing resilience under changing climates and fire regimes in USA forests Fire and forests in the 21st century: Managing resilience under changing climates and fire regimes in USA forests

Higher temperatures, lower snowpacks, drought, and extended dry periods have contributed to increased wildfire activity in recent decades. Climate change is expected to increase the frequency of large fires, the cumulative area burned, and fire suppression costs and risks in many areas of the USA. Fire regimes are likely to change due to interactions among climate, fire, and other...
Authors
James M. Vose, David L. Peterson, Christopher J. Fettig, Jessica E. Halofsky, J. Kevin Hiers, Robert E. Keane, Rachel A. Loehman, Michael C. Stambaugh

The Mount Hood fault zone, active faulting at the crest of the dynamic Cascade Range, north-central Oregon, USA The Mount Hood fault zone, active faulting at the crest of the dynamic Cascade Range, north-central Oregon, USA

The Mount Hood fault zone is a N-trending, ~55-km-long zone of active faulting along the western margin of the Hood River graben in north-central Oregon. The Mount Hood fault zone occurs along the crest of the Cascade Range and consists of multiple active fault segments. It is presently unclear how much Hood River graben extension is actively accommodated on the fault zone, and how...
Authors
Ian Madin, Ashley R. Streig, Scott E.K. Bennett

Arc versus river: The geology of the Columbia River Gorge Arc versus river: The geology of the Columbia River Gorge

The Columbia River Gorge is the Columbia River’s long-held yet evolving passage through the volcanic arc of the Cascade Range. The globally unique setting of a continental-scale river bisecting an active volcanic arc at the leading edge of a major plate boundary creates a remarkable setting where dynamic volcanic and tectonic processes interact with diverse and energetic fluvial...
Authors
Jim E. O'Connor, Ray Wells, Scott E.K. Bennett, Charles M. Cannon, Lydia M. Staisch, James L Anderson, Anthony Francis Pivarunas, Gabriel Wells Gordon, Richard J. Blakely, Mark E. Stelten, Russell C. Evarts

Paleozoic and Mesozoic tectonic events west of the Waterbury Dome: Results of new mapping in the western Connecticut Highlands Paleozoic and Mesozoic tectonic events west of the Waterbury Dome: Results of new mapping in the western Connecticut Highlands

This field trip highlights the results of recent U.S. Geological Survey (USGS) bedrock geologic mapping in four 7.5 min quadrangles in the western Connecticut highlands near Southbury, Connecticut, USA. The rocks are broadly within what Rodgers (1985) called the Hartland and Gneiss Dome belts of the Connecticut Valley Synclinorium (Rodgers, 1985; Fig. 1), the latter of which is now known...
Authors
William C. Burton, William J. Devlin

Upper Grand Coulee: New views of a channeled scabland megafloods enigma Upper Grand Coulee: New views of a channeled scabland megafloods enigma

New findings about old puzzles occasion rethinking of the Grand Coulee, greatest of the scabland channels. Those puzzles begin with antecedents of current upper Grand Coulee. By a recent interpretation, the upper coulee exploited the former high-level valley of a preflood trunk stream that had drained to the southwest beside and across Coulee anticline or monocline. In any case, a...
Authors
Richard B. Waitt, Brian F. Atwater, Karin Lehnigk, Isaac J. Larsen, Bruce N. Bjornstad, Michelle A. Hanson, Jim E. O'Connor

Developing landslide chronologies using landslide-dammed lakes in the Oregon Coast Range Developing landslide chronologies using landslide-dammed lakes in the Oregon Coast Range

The Oregon Coast Range is a dynamic landscape that is continually shaped by shallow and deep-seated landslides that can have disastrous consequences to infrastructure and human lives. Searching for evidence of potentially coseismic mass wasting is incredibly difficult, particularly when historical observations are limited. Landslide-dammed lakes with submerged “ghost forests” in the...
Authors
Logan Wetherell, William Struble, Sean Richard LaHusen

Hypogenic karst of the Great Basin Hypogenic karst of the Great Basin

Discoveries in the 1980s greatly expanded speleologists’ understanding of the role that hypogenic groundwater flow can play in developing caves at depth. Ascending groundwater charged with carbon dioxide and, especially, hydrogen sulfide can readily dissolve carbonate bedrock just below and above the water table. Sulfuric acid speleogenesis, in which anoxic, rising, sulfidic groundwater...
Authors
Louise D. Hose, Harvey R. DuChene, Daniel Jones, Gretchen M. Baker, Zoe Havlena, Donald S. Sweetkind, Doug Powell

Frequency distribution Frequency distribution

Given a numerical dataset, a frequency distribution is a summary displaying fluctuations of an attribute within the range of values. In contrast to an analytical probability distribution, a frequency distribution always deals with empirically observed values (Everitt and Skondall 2010). In general, the larger the number of values, the more useful is the frequency distribution relative to...
Authors
Ricardo A. Olea
Was this page helpful?