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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: 6197

Workshop summary, conclusions and recommendations Workshop summary, conclusions and recommendations

No abstract available.
Authors
W.H. Benson, R.T. Di Giulio, D. E. Tillitt, L. Birnbaum, P.L deFur, Jay W. Gooch, Ellen Mihaich, C. Tyler

Characterizing fractured-zone flow using numerical flow-log models Characterizing fractured-zone flow using numerical flow-log models

Water-quality monitoring and hydraulic testing in fractured bedrock aquifers involves two important tasks: 1) identifying the hydraulically active fractures intersecting the borehole, and 2) inferring how the specific entry or exit ports in the borehole wall are connected to large-scale flow paths in the region surrounding the borehole. Effective characterization of fractured bedrock...
Authors
Frederick L. Paillet

Yellowstone bears Yellowstone bears

No abstract available.
Authors
R.R. Knight, B.M. Blanchard, P. Schullery

Potassium-calcium decay system Potassium-calcium decay system

Potassium has three isotopes (see Potassium); potassium-40 ( 40K) is radioactive and decays to both calcium-40 ( 40Ca) and argon-40 ( 40Ar). The combined half-life of 40K is 1.25 billion years. The branched decay scheme of 40K is shown in Figure P33. It decays by β- decay to 40Ca and to 40Ar by both electron capture and positron decay (see Potassium-argon decay system). Although 89.52%...
Authors
Brian D. Marshall

Dating methods Dating methods

One of the greatest contributions of geochemistry to man's knowledge of the Earth and solar system has been the development and application of chemical and isotopic techniques used to measure the passage of time. Rates of geologic processes, rates of biological evolution, and contemporaneity of past events all depend on accurate ages of geologic materials. Many geochemical methods have...
Authors
Brian D. Marshall

Continental diatoms as indicators of long-term environmental change Continental diatoms as indicators of long-term environmental change

It is curious that diatoms, whose short lifespans and capacity for rapid regeneration make them especially suitable for short-term paleoenvironmental studies, would also have a significant role as indicators of long-term environmental change. This chapter explores the nature of long diatom records, their relation to global environmental changes, guidelines for their interpretation, and...
Authors
J. Platt Bradbury

Laramide to Holocene structural development of the northern Colorado Front Range Laramide to Holocene structural development of the northern Colorado Front Range

The Rocky Mountain province of the United States is a classic basement-involved foreland orogen. Deformation during the Late Cretaceous to Eocene Laramide orogeny created an anastomosing system of basement-cored arches that bound the northern and eastern margins of the Colorado Plateau and the elliptical sedimentary basins of the Rockies. The tectonic mechanism for Laramide deformation...
Authors
Eric A. Erslev, Karl S. Kellogg, Bruce Bryant, Timothy K. Ehrlich, Steven M. Holdaway, Charles W. Naeser
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