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: 6063

Development of slope valleys in the glacimarine environment of a complex subduction zone, Northern Gulf of Alaska

Morphological, seismic-reflection, and sedimentological evidence indicates that glacial ice tongues cut large sea valleys into the Gulf of Alaska continental shelf during the Pleistocene. During the Holocene, glacially-derived sediments from the Copper River and other meltwater streams have been prograding seaward across the shelf, covering the glacial and glacimarine upper Yakataga diamicts that
Authors
Paul R. Carlson, Terry R. Bruns, Michael A. Fisher

Chapter 22: Changing patterns of extensional tectonics; Overprinting of the basin of the middle and upper Miocene Esmeralda Formation in western Nevada by younger structural basins

The middle and upper Miocene Esmeralda Formation of western Nevada was deposited in a continental basin that crops out over an area of about 2,000 km2. The formation consists of thin, westerly derived sedimentary rocks in the western three-quarters of the outcrop area and of thick (3+ km) easterly derived sedimentary rocks in the eastern quarter. Megabreccias along the eastern margin of the basin
Authors
John H. Stewart, David S. Diamond

Chapter 10: Shallow crustal deformation in the Pahranagat area, southern Nevada

The Pahranagat area lies in the Basin and Range Province of southern Nevada. Paleozoic rocks in the study area were folded and faulted during the Sevier orogeny and subsequently extended prior to deposition of Tertiary strata. Middle Oligocene strata overlie the Paleozoic rocks with pronounced angular unconformity and were deposited on rocks of Late Cambrian through Pennsylvanian age in the easter
Authors
Angela S. Jayko

Chapter 6: Petrogenesis of the composite peraluminous-metaluminous Old Woman-Piute Range batholith, southeastern California; isotopic constraints

The Late Cretaceous Old Woman–Piute Range batholith includes both metaluminous and strongly peraluminous granitoid series that intruded the reactivated craton of southeastern California shortly after the orogenic peak. Whole-rock Sr, Nd, and O, feldspar Pb, and zircon U-Pb isotopic compositions, in combination with major- and trace-element and petrographic data, indicate that although these series
Authors
Calvin F. Miller, Joseph L. Wooden, Victoria C. Bennett, James E. Wright, G. Cleve Solomon, Richard W. Hurst

The effect of developmental activities on water quality functions of bottomland hardwood ecosystems: the report of the water quality workgroup

No abstract available.
Authors
M.L. Scott, B.A. Kleiss, W.H. Patrick, C.A. Segelquist

The calculation of flushing flows for gravel and cobble bed rivers

No abstract available.
Authors
Robert T. Milhous

Introduction

No abstract available.
Authors
J. E. Roelle, Gregor T. Auble, J. G. Gosselink

Mammals of La Selva, Costa Rica

No abstract available.
Authors
Don E. Wilson

Altered flows and created landscapes in the Platte River Headwaters, 1840-1990

No abstract available.
Authors
Fritz L. Knopf, Michael L. Scott

Human activities and ecological processes in bottomland hardwood ecosystems: the report of the Ecosystem Workgroup

No abstract available.
Authors
J. G. Gosselink, M.M. Brinson, L.C. Lee, Gregor T. Auble

Embryotoxicity and teratogenicity of environmental contaminants to bird eggs

In light of recent ecological disasters such as the Exxon Valdez oil spill of 1989, which has already claimed the lives of thousands of aquatic birds with the reproductive success of countless others at risk, there is a need to evaluate the embryotoxic potential of a continuously growing number of industrial and agricultural environmental contaminants that may come in direct contact with bird eggs
Authors
David J. Hoffman

The California Valley grassland

Grasslands are distributed throughout California from Oregon to Baja California Norte and from the coast to the desert (Brown 1982) (Figure 1). This review will focus on the dominant formation in cismontane California, a community referred to as Valley Grassland (Munz 1959). Today, Valley Grassland is dominated by non-native annual grasses in genera such as Avena (wild oat), Bromus (brome grass)
Authors
J. E. Keeley