Publications
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Identifying sources of aeolian mineral dust: Present and past Identifying sources of aeolian mineral dust: Present and past
Aeolian mineral dust is an important component of the Earth’s environmental systems, playing roles in the planetary radiation balance, as a source of fertilizer for biota in both terrestrial and marine realms and as an archive for understanding atmospheric circulation and paleoclimate in the geologic past. Crucial to understanding all of these roles of dust is the identification of dust...
Authors
Daniel R Muhs, Joseph M Prospero, Matthew C Baddock, Thomas E Gill
230Th/U ages Supporting Hanford Site‐Wide Probabilistic Seismic Hazard Analysis 230Th/U ages Supporting Hanford Site‐Wide Probabilistic Seismic Hazard Analysis
This product represents a USGS Administrative Report that discusses samples and methods used to conduct uranium-series isotope analyses and resulting ages and initial 234U/238U activity ratios of pedogenic cements developed in several different surfaces in the Hanford area middle to late Pleistocene. Samples were collected and dated to provide calibration of soil development in surface...
Authors
James B. Paces
Evidence of repeated wildfires prior to human occupation on San Nicolas Island, California Evidence of repeated wildfires prior to human occupation on San Nicolas Island, California
Understanding how early humans on the California Channel Islands might have changed local fire regimes requires a baseline knowledge of the frequency of natural wildfires on the islands prior to human occupation. A sedimentary sequence that was recently discovered in a small canyon on San Nicolas Island contains evidence of at least 24 burn events that date to between ∼37 and 25 ka...
Authors
Jeffrey S. Pigati, John P. McGeehin, Gary L. Skipp, Daniel R. Muhs
High-resolution topography and geomorphology of select archeological sites in Glen Canyon National Recreation Area, Arizona High-resolution topography and geomorphology of select archeological sites in Glen Canyon National Recreation Area, Arizona
Along the Colorado River corridor between Glen Canyon Dam and Lees Ferry, Arizona, located some 25 km downstream from the dam, archaeological sites dating from 8,000 years before present through the modern era are located within and on top of fluvial and alluvial terraces of the prehistorically undammed river. These terraces are known to have undergone significant erosion and retreat...
Authors
Brian D. Collins, Skye C. Corbett, Joel B. Sankey, Helen C. Fairley
Correlated patterns in hydrothermal plume distribution and apparent magmatic budget along 2500 km of the Southeast Indian Ridge Correlated patterns in hydrothermal plume distribution and apparent magmatic budget along 2500 km of the Southeast Indian Ridge
Multiple geological processes affect the distribution of hydrothermal venting along a mid-ocean ridge. Deciphering the role of a specific process is often frustrated by simultaneous changes in other influences. Here we take advantage of the almost constant spreading rate (65–71 mm/yr) along 2500 km of the Southeast Indian Ridge (SEIR) between 77°E and 99°E to examine the spatial density...
Authors
Edward Baker, Christophe Hemond, Anne Briais, Marcia Maia, Daniel S. Scheirer, Sharon L. Walker, Tingting Wang, Yongshun John Chen
Geologic framework of thermal springs, Black Canyon, Nevada and Arizona Geologic framework of thermal springs, Black Canyon, Nevada and Arizona
Thermal springs in Black Canyon of the Colorado River, downstream of Hoover Dam, are important recreational, ecological, and scenic features of the Lake Mead National Recreation Area. This report presents the results from a U.S. Geological Survey study of the geologic framework of the springs. The study was conducted in cooperation with the National Park Service and funded by both the...
Authors
L. Sue Beard, Zachary W. Anderson, Tracey J. Felger, Gustav B. Seixas
Preliminary geologic map of Black Canyon and surrounding region, Nevada and Arizona Preliminary geologic map of Black Canyon and surrounding region, Nevada and Arizona
Thermal springs in Black Canyon of the Colorado River, downstream of Hoover Dam, are important recreational, ecological, and scenic features of the Lake Mead National Recreation Area. This report presents the results from a U.S. Geological Survey study of the geologic framework of the springs. The study was conducted in cooperation with the National Park Service and funded by both the...
Authors
Tracey J. Felger, L. Sue Beard, Zachary W. Anderson, Robert J. Fleck, Joseph L. Wooden, Gustav B. Seixas
Historical channel-planform change of the Little Colorado River near Winslow, Arizona Historical channel-planform change of the Little Colorado River near Winslow, Arizona
This study evaluates channel-planform adjustment on an alluvial reach of the Little Colorado River and documents the geomorphic evolution of the channel through an analysis of aerial photographs and orthophotographs for the period 1936–2010. The Little Colorado River has adjusted to the effects of an extreme flood in 1923 and a subsequent decline in peak discharge and mean annual flow by...
Authors
Debra L. Block
Preliminary geologic map of the eastern Willapa Hills, Cowlitz, Lewis, and Wahkiakum Counties, Washington Preliminary geologic map of the eastern Willapa Hills, Cowlitz, Lewis, and Wahkiakum Counties, Washington
This digital map database and the PDF derived from the database were created from the analog geologic map: Wells, R.E. (1981), “Geologic map of the eastern Willapa Hills, Cowlitz, Lewis, and Wahkiakum Counties, Washington.” The geodatabase replicates the geologic mapping of the 1981 report with minor exceptions along water boundaries and also along the north and south map boundaries...
Authors
Ray E. Wells, Michael G. Sawlan
Identifying dominant controls on hydrologic parameter transfer from gauged to ungauged catchments: a comparative hydrology approach Identifying dominant controls on hydrologic parameter transfer from gauged to ungauged catchments: a comparative hydrology approach
Daily streamflow information is critical for solving various hydrologic problems, though observations of continuous streamflow for model calibration are available at only a small fraction of the world’s rivers. One approach to estimate daily streamflow at an ungauged location is to transfer rainfall–runoff model parameters calibrated at a gauged (donor) catchment to an ungauged (receiver...
Authors
R. Singh, S.A. Archfield, T. Wagener
Comments on the Yule Marble Haines block: Potential replacement, Tomb of the Unknown Soldier, Arlington National Cemetery Comments on the Yule Marble Haines block: Potential replacement, Tomb of the Unknown Soldier, Arlington National Cemetery
Marble for the Tomb of the Unknown Soldier at Arlington National Cemetery was cut from the Colorado Yule Marble Quarry in 1931. Although anecdotal reports suggest that cracks were noticed in the main section of the monument shortly after its installation at the Arlington National Cemetery in Arlington, Virginia, detailed documentation of the extent of cracking did not appear until 1963...
Authors
Victor G. Mossotti
Key subsurface data help to refine Trinity aquifer hydrostratigraphic units, south-central Texas Key subsurface data help to refine Trinity aquifer hydrostratigraphic units, south-central Texas
The geologic framework and hydrologic characteristics of aquifers are important components for studying the nation’s subsurface heterogeneity and predicting its hydraulic budgets. Detailed study of an aquifer’s subsurface hydrostratigraphy is needed to understand both its geologic and hydrologic frameworks. Surface hydrostratigraphic mapping can also help characterize the spatial...
Authors
Charles D. Blome, Allan K. Clark